GEOLOGICA CARPATHICA
, AUGUST 2018, 69, 4, 315–334
doi: 10.1515/geoca-2018-0019
www.geologicacarpathica.com
A calcite crisis unravelling Early Miocene (Ottnangian)
stratigraphy in the North Alpine–Carpathian Foreland
Basin: a litho- and chemostratigraphic marker
for the Rzehakia Lake System
MARKUS PALZER-KHOMENKO
1,
, MICHAEL WAGREICH
1
, WOLFGANG KNIERZINGER
1
,
MARIA MESZAR
1
, SUSANNE GIER
1
, MĂDĂLINA–ELENA KALLANXHI
2
and ALI SOLIMAN
3
1
Department of Geodynamics and Sedimentology, University of Vienna, Althanstraße 14, 1090 Wien, Austria;
markus.palzer@gmx.at,
michael.wagreich@univie.ac.at, knierz@gmail.com, maria.meszar@univie.ac.at, susanne.gier@univie.ac.at
2
Department of Geology. Faculty of Biology and Geology, Babeş-Bolyai University, Str. Mihail Kogălniceanu 1, Cluj-Napoca 400084,
Romania; madalina_kallanxhi@yahoo.com
3
Geology Department, Faculty of Science, Tanta University, Tanta 31527, Egypt; ali.soliman@science.tanta.edu.eg
(Manuscript received December 21, 2017; accepted in revised form May 31, 2018)
Abstract: Within the Lower Austrian part of the North Alpine Foreland Basin (NAFB), up to 1000 m of sediments were
deposited throughout the Ottnangian (Early Miocene, Burdigalian). According to homogeneous compositions and sparse
biostratigraphic resolution, a consistent stratigraphic concept from the basin margins into the foreland depocenter was
still lacking. New investigations on several deep drill cores throughout the basin provide comprehensive sedimentological,
mineralogical, chemical and micropaleontological data. A calcite poor, fossil- and pyrite-free, smectite-rich, up to 800 m
thick interval was identified and correlated to the time interval of the late Ottnangian brackish Rzehakia Lake System. For
this section, we introduce the term Calcite Minimum Interval (CMI). We define the onset of the CMI by a sharp decrease
of calcite contents and the disappearance of autochthonous (and reworked) calcareous nannofossils. We define the termi-
nation of the CMI by the permanent increase of pyrite contents and the reappearance of calcareous nannofossils. The CMI
as a litho- and chemostratigraphical marker for the Rzehakia Lake System constitutes a stratigraphic key horizon. Within
the NAFB in Lower Austria, its onset corresponds to the middle/upper Ottnangian transition while its termination
correlates roughly to the Ottnangian / Karpatian boundary. This allows a precise definition, identification and correlation
of (upper) Ottnangian stratigraphic units of the NAFB. For the central basinal parts of the Rzehakia Lake System, we
introduce the new lithostratigraphic term Wildendürnbach Formation which correlates to the marginal Traisen Formation.
Keywords: Stratigraphy, Early Miocene, late Ottnangian, Molasse Basin, Rzehakia Lake System, Calcite Minimum
Interval.
Introduction
Stratigraphic correlation in foreland basins such as the Northern
Alpine Foreland Basin (NAFB, Rasser et al. 2008) is often
hampered by restricted marine environments, frequent and
diachronous marine–non-marine facies changes due to tecto-
nic control on regional subsidence and uplift, and the lack of
basin-wide synchronous stratigraphic events (e.g., Harzhauser
& Mandic 2008; Kováč et al. 2017; Sant et al. 2017b). Although
the large-scale stratigraphic geometry and succession of fore-
land basins follow process-based first-principle models (e.g.,
Sinclair & Allen 1992; Sinclair 1997; Sissingh 1997) gover-
ned by flexural subsidence due to foreland-propagating oroge-
nic loading and the evolution from underfilled (deep-marine)
to overfilled (marginal marine-limnic) phases (Allen et al.
1991), detailed stratigraphic correlations and the identification
of synchronous basin-wide markers pose a major problem
(Sant et al. 2017b). Magnetostratigraphy and absolute dating
of tuffs have improved correlations for parts of the NAFB
from Austria to Switzerland (e.g., Schlunegger et al. 1996;
Nehyba & Roetzel 1999; Reichenbacher et al. 2013; Roetzel et
al. 2014; Sant et al. 2017a). Short regional climatic events
(e.g., Böhme et al. 2008) expressed in the basin fill may pro-
vide a way for detailed correlation, with astronomical tuning
providing means for establishing high-resolution time frames
(Abdul Aziz et al. 2003).
Here we use litho- and chemostratigraphical approaches to
unravel a prominent signal of reduced calcite contents at the
transition from the NAFB to the Carpathian foredeep in Lower
(eastern) Austria and link it to the Burdigalian sea-level low-
stand and the corresponding late Ottnangian Rzehakia Lake
System, a distinct depositional phase of the NAFB (Čtyroký
1968; Mandic & Ćorić 2007; Harzhauser & Mandic 2008).
The stratigraphy in the study area was so far only resolved in
low resolution and rather poorly defined in modern lithostrati-
graphic terms due to poor outcrop conditions as well as the lack
of distinctive microfossils and magnetostratigraphic studies
(e.g., Roetzel et al. 1999a, 2006; Ćorić & Roegl 2004; Piller
et al. 2004, 2007; Wessely 2006; Mandic & Ćorić 2007;
Harzhauser & Mandic 2008; Gebhardt et al. 2013). Although
a large number of wells were drilled by the petroleum industry
especially in the 1960s to 1980s, stratigraphic concepts and
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, 2018, 69, 4, 315–334
correlations remained dubious and contradictory (e.g.,
Aniwandter et al. 1990; Hamilton 1997; Mandic & Ćorić
2007; Harzhauser & Mandic 2008; Gebhardt et al. 2013;
Kováč et al. 2017; Sant et al. 2017b). Based on chemical and
mineralogical data, a prominent and traceable event signal can
be identified which constitutes a new tool to correlate syn-
chronous deposits throughout the Lower Austrian Molasse
Basin (LAMB) and to the Western Carpathians. We rely on
correlations of industry well data with the surface geology
to set up a modified lithostratigraphic concept for the late
Ottnangian Lower Austrian part of the NAFB, the LAMB and
its correlations to the west and east.
Geological setting
The easternmost part of the NAFB, the Lower Austrian
Molasse Basin (LAMB), is situated at the transition to
the Carpathian Foreland Basin and the Vienna Basin between
the Bohemian Massif to the NW, the Alpine orogen to the S,
and the Western Carpathian fold-and-thrust belt to the NE. It is
part of the Central Paratethys paleogeographic realm (Fig. 1;
Roegl & Steininger 1983).
During the Early Miocene (Burdigalian, Eggenburgian–
Karpatian of the regional Central Paratethys stratigraphy, e.g.,
Piller et al. 2007; Krijgsman & Piller 2012), up to 2000 m of
clastic pelitic and sandy sediments (as can be identified in
the well Laa 1), often referred to as “Schlier”, were deposited
in the study area. These sediments show a homogeneous mine-
ralogical and chemical composition. According to poor bio-
stratigraphical resolution, the internal differentiation and
correlations to Molasse successions to the west (e.g., Upper
Austria and Bavaria, Rupp et al. 2008; Heckeberg et al. 2010;
Reichenbacher et al. 2013; Pippèrr & Reichenbacher 2017;
Sant et al. 2017b) and (north-) east (e.g., Čtyroký 1972;
Čtyroký et al. 1973; Holcová 2001, 2002; Krhovský et al.
2001; Kováč et al. 2004, 2017; Šikula & Nehyba 2004)
remained questionable. Additional problems arise, as the
Ottnan gian is subdivided into a marine lower and middle and
a brackish upper Ottnangian in the west by use of benthic
fora minifers (e.g., Rupp et al. 2008; Grunert et al. 2010a;
Pippèrr & Reichenbacher 2017; Sant et al. 2017a). This subdi-
vision is rarely aplicable for the LAMB where poor micro-
fossil content and biostratigraphic resolution makes a precise
chronostratigraphic attribution more challenging. Especially
the distinction of a lower and middle Ottnangian remains
Fig. 1. Geological map of the study area in Lower Austria and investigated wells. Compilation of maps by Wessely (2006) and Schuster et al.
(2015).
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undefined regarding modern chronostratigraphy. Piller et al.
(2007) describes the Ottnangian in the NAFB as a “strictly
twofold stage with a normal marine development in its lower
part and a predominance of restricted marine to fresh water
environments in its upper part” (Piller et al. 2007, p. 155).
Čtyroký (1968) already described the occurrence of brackish
Rzehakia Beds or Series from Switzerland to the Caspian
region. Harzhauser & Mandic (2008) defined the brackish
Rzehakia Lake System which prevailed during the late
Ottnangian in the sense of Piller et al. (2007).
The overview map (Fig. 1) based on Wessely (2006) shows
the distribution of the lower Ottnangian “Robulus Schlier s.l.
(sensu lato)” (Piller et al. 2004) at the southeastern rim of
the LAMB. To the north, it is overlain by massive decalcified
micaceous Ottnangian sands of the Traisen Fm. (Formation).
The Traisen Fm. was defined by Gebhardt et al. (2013) and
comprises the former outcropping Oncophora sands in Lower
Austria south of the Danube. North of the Danube, the Traisen
Fm. is overlain by the Karpatian Laa Fm. (Roegl et al. 1997).
In contrast to the decalcified Traisen Fm., the calcareous Laa
Fm. bears a distinct marine microfauna (Roetzel et al. 1999a,
2009; Roegl et al. 2002; Ćorić & Roegl 2004).
The Ottnangian north of the Danube is represented by
the Zellerndorf Fm. (Roetzel et al. 1999c, 2006; Piller et al.
2004), which crops out at the NW rim of the LAMB to
the Bohemian Massif. It is also overlain by the Karpatian
Laa Fm. The delimitation of the Zellerndorf Fm. in the NW to
the Traisen Fm. and the “Robulus Schlier” in the S is so far
undefined. Whether the Zellerndorf Fm. correlates to
the Traisen Fm., to the “Robulus Schlier s.l.” or to both
remains unsolved.
While numerous investigations where conducted on surface
outcrops close to the Bohemian Massif in the NW and
the Alpine front in the S (Roetzel 1991, 1992, 1994; Roetzel et
al. 1999b, 2006; Roegl et al. 2002; Wessely 2006; Mandic &
Ćorić 2007; Grunert et al. 2010b; Nehyba & Roetzel 2010;
Wimmer-Frey et al. 2013; Gebhardt et al. 2014), the central
and subsurface parts of the LAMB remained mostly uncharted
except for oil industry internal reports (OMV AG, RAG) and
few published papers (Aniwandter et al. 1990; Hamilton 1997;
Ćorić & Roegl 2004). Consequently, the correlation of Ottnan-
gian deposits throughout the LAMB remains challenging.
In addition, sparse biostratigraphical resolution, high sedi-
mentation rates and the absence of microfossils in large parts
of the Ottnangian deposits complicate the development of
a consistent (litho-) stratigraphic model in the LAMB.
Material and methods
Seven wells in a SW–NE transect throughout the LAMB
were chosen for detailed investigations. Data of the more
complete five wells are presented hereinafter: Schaubing
(water well, data courtesy by Austrian Geological Survey),
Streithofen 1, Altenmarkt im Thale 1, Laa 1 and Wilden-
dürnbach K4 (Fig. 1; all well data except Schaubing courtesy
of OMV AG). While the shallow (140 m) well of Schaubing
offered a continuous core, all other wells provide 3–5 m long
drill-cores with gaps of 50–200 m in between. Drill cutting
samples were taken from these uncored intervals were neces-
sary. A total of 280 drill core samples and additional 164 sam-
ples of cuttings were analyzed.
The carbonate-content was measured by a Carbonate Bomb
(Mueller & Gastner 1971). A certain amount of sample-
powder was placed in the Carbonate Bomb. The Bomb was
closed and the sample-powder was mixed with 25% hydro-
chloric acid, which reacted with carbonate. The resulting CO
2
increased the air-pressure which was measured and allowed
the determination of the carbonate content.
The bulk mineralogy was analyzed by X-ray diffraction
(XRD) on oriented powders by a Panalytical X’Pert PRO dif-
fractometer (CuKα radiation, 40 kV, 40 mA, step size 0.0167,
5 s per step). Semi-quantitative information was extracted by
using peak intensities as counts per second (cps) of characte-
ristic peaks with low or without overlapping problems with
other minerals. Background values were subtracted from peak
heights.
Dry powders were analyzed by a Bruker AXS TRACER
IV-SD handheld Energy Dispersive X-ray Fluorescence
(ED-XRF) instrument. The measured cps were used for infer-
ring semiquantitative trends calibrated to internal quantitative
data, for which elements/oxides were determined by ICP-MS
by the ACME-Labs (now Bureau Veritas) in Vancouver/
Canada.
For nannofossil analyses on 169 samples, smear slides were
prepared according to the standard smear slide technique of
Bown & Young (1998). The samples were analyzed using
a Leica DM 2700P microscope (×1000 magnification) in
parallel (bright field — BF) and crossed polarized light (XPL).
The microphotographs were captured with a Leica MC170
HD camera. Relative abundance / sample
was assessed as fol-
lows: A — Abundant (21–50 specimens / Field of View FOV),
C — Common (11–20 specimens / FOV), F — Few (1–10
speci mens / FOV), R — Rare (1–10 specimens / 10 FOV),
VR — Very rare (1 specimen / >11 FOV) and B — barren of
nannofossils. Preservation was noted with G — good, M —
moderate and P — poor. We refer here to the standard zona-
tions of Martini (1971) and Okada & Bukry (1980), based on
the First Occurrence (FO) and Last Occurrence (LO) of
the zonal markers species. 50 samples were chosen for organic
walled dinoflagellate cysts. The sample preparation method is
described in Soliman (2012). Data were imported to a rela-
tional access database allowing for combined analyses.
Excerpts of this database are presented here.
Results
Wildendürnbach Formation
To solve the problems and contradictions concerning
the cor relation of Ottnangian deposits, (especially the former
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outdated term “Oncophora Beds”), we hereby introduce a new
lithostratigraphic unit, the Wildendürnbach Fm. It represents
the upper Ottnangian deposits of the Rzehakia Lake System in
the central LAMB. The detailed formalization and definition
of the herein newly defined Wildendürnbach Fm. can be found
in Appendix A.
Formerly used terms are inapropriate for the deposits of
the Wildendürnbach Fm. The term “Robulus Schlier s.l.” (as
an extension of the term “Robulus Schlier s. str.” in Upper
Austria) is poorly defined in Lower Austria and usually com-
prises calcareous pelitic depo sits with a marine fauna. The Traisen
Fm. is precisely defined from outcrop studies and includes
proximal, massive sands exposed in the southern parts of
the basin (Gebhardt et al. 2013). The Zellerndorf Fm. includes
an interval of calcareous marine pelites and comprises all of
the Ottnangian (and even the upper Eggenburgian, e.g., Roetzel
et al. 1999a, 2006, 2014). “Oncophora Beds” is a widely and
sometimes erro neously used term, e.g., for strata without any
sign of the bivalve “Oncophora” or “Rzehakia” (Aniwandter
et al. 1990; Čtyroký 1972; Gebhardt et al. 2013; Hamilton 1997).
The term “Fisch Fazies” usually used in petroleum industry
well profile descriptions is poorly defined, not described in
surface outcrops and unknown to many surface geologists.
Well descriptions
The 144 m deep well Schaubing (SCHB, Fig. 2) offers
a continuous 144 m long drill core section from the crystalline
basement to the surface. The basal Bohemian Massiv granu-
lites are overlain by a conglomerate and monotonous carbo-
nate-rich silts interlayered with coarse-grained sands of
reworked granulites. From 112 m upwards, marly silts rich in
fish-scales become frequent. At 72 m, a bed of fine-grained
micaceous sands interrupts the pelites and is followed by
a carbonate-poor clay layer of 5 m thickness. The clastic input
starts to increase at 40 m. Massive sands interrupted by car-
bonate-cemented sandstones dominate above 25 m.
The 1300 m deep well Streithofen 1 (STRTH-1) comprises
a profile of 3–5 m thick drill core sections every 50 m (except
in the uppermost 300 m) from the surface to the crystalline
basement. The crystalline basement is overlain by quartz rich
sandstones and coaly clay to siltstones. The coaly beds are
tecto nically fractured and show pieces of polished slicken-
sides. At 1120 m, strongly bioturbated bluish sandstones
occur. At 1100 m, they are overlain by the typical “Schlier”
succession of layered muddy clay, silt and sandstones. Sands
show partly erosional bases and planar lamination, but struc-
tureless massive sand layers dominate. A decrease in carbo-
nate content was recognized at 850 m. Self-Potential-Logs
indicate the increase of coarse clastic sediments at 780 m.
The upper 800 m are dominated by micaceous, massive sand
packages interrupted by carbonate cemented layers, fining
upward cycles, rip up clasts, planar laminations and convolute
bedding. Few pelitic interlayers were detected.
The 3200 m deep well of Altenmark T1 (ALT-T1) offers
3–5 m thick drill core sections every 100–200 m. Cutting
samples were taken every 30–50 m to fill the gaps. At 1205 m,
a breccia of (Mesozoic?) carbonate clasts and a sandy matrix
is discordantly overlain by a strongly bioturbated sandstone.
From 1070 m to 530 m, light grey micaceous sands with partly
turbiditic structures grading into yellowish to brownish muds,
dominate the drill cores. These sands are interrupted by
bluish-grey, mm-laminated shale. Self-Potential-Logs indicate
pelitic intervals interrupting the turbiditic succession at
790–735 m and 690–675 m. At 505 m, yellowish muds occur.
Two drill core sections of good preservation from the 3100 m
deep well Laa 1 (1633–1638 m; 1794–1799 m) were available.
The cores show turbiditic structures and were dominated by
light grey micaceous sands and brownish muds and muddy
sands containing numerous clay clasts. Many erosional sur-
faces are present. A bluish-grey, mm-laminated shale consti-
tutes the background sedimentation. Plant fragments and fish
scales commonly occur. Cuttings and Self-Potential-Logs indi-
cate a homogeneous pelitic sedimentation from 1945–1550 m
followed by a turbiditic sand-dominated sedimentation up to
935 m interrupted by several pelitic intervals (1400–1356 m;
1275–1250 m; 1190–1170 m).
The 2600 m deep well of Wildendürnbach K4 (WDK-4;
Fig. 3) offeres a large number of 3–5 m thick cored sections.
Unfortunately, 20–80 % of the original material is missing.
Most cores are unsorted and the origin of several pieces is
questionable according to divergent drill core diameters.
Nevertheless, the overall characteristics can be recognized.
Below 1500 m, strongly bioturbated fine-grained and massive
sands occur. Fish scales are common. Between 1500–1250 m
(supported by Self-Potential-Logs), a bluish-grey, pelitic
background sedimentation interrupted by turbiditic sands and
few debris flows or slumps occur. The turbiditic sands become
more frequent to the top. According to Self-Potential-Logs
and drill cores, the amount of sands and muds strongly
increases between 1250–1135 m, while pelites dominate
between 1135–1045 m. Up to 800 m, massive sand dominated
intervals alternate with pelitic intervals. At 750 m, the sedi-
ments are again dominated by pelites. The turbiditic sands are
light grey, micaceous and carbonate bearing and contain clay
clasts and plant remnants. The mm-laminated bluish-grey
pelites usually contain fish scales and offer changing carbo-
nate contents.
Micropaleontology
101 of the 169 samples proved to be barren of nannofossils,
and 26 yielded only few individuals. These samples were inves-
tigated only qualitatively (presence/absence data). The cal ca-
reous nannofossil association is highly diverse and contains
well to poorly preserved specimens (Fig. 4; Appendix B for
full taxonomic list and Appendix C “Calcareous Nannofossil
Data”). In general, the species belonging to the autochthonous
assemblage are better preserved than the reworked ones. In this
study, the long ranging taxa such as: Coccolithus pelagicus,
Cyclicargolithus floridanus, Reticulofenestra minuta and
Braarudosphaera bigelowii were considered as being part of
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Fig.
2.
The
sedimentary
log
of
the
well
of
Schaubing
of
fers
a
pelitic
marly
lower
part
(up
to
70
m)
and
a
general coarsening upward trend above.
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the autochthonous assemblage. The assemblage contains 46
species, being dominated by: Coccolithus pelagicus,
Reticulofenestra minuta, R. pseudoumbilicus, Helicosphaera
ampliaperta, Syracosphaera spp. (S. cf. pulchra and S. cf.
oneillii), R. haqii, Coronosphaera mediterranea and Braa rudo
sphaera bigelowii. Rare to very rare presence have Acanthoica
sp., Calcidiscus spp., Coronocyclus spp., Cyclicargolithus
floridanus, Discoaster spp., Helicosphaera mediterranea,
H. carteri, H. scissura, H. vedderi, Helicosphaera sp.,
Hughesius tasmaniae, Pontosphaera multipora, Reticulo
fenestra ampliumbilicus, R. gelida, Sphenolithus spp., Triquet
rorhabdulus sp., Thoracosphaera sp., Umbilicosphaera jafari
and U. rotula. Other species with rare occurrence can be seen
in Appendix B.
Intervals lacking nannofossils occurred in all wells
(Appendix D). In the well of Schaubing, all samples above
80 m depth were barren. In the well of Streithofen 1, all except
three samples above 855 m depth were barren. The samples at
853.8 m, 654.8 m and 151.5 m contained only few specimens.
The well of Altenmarkt T1 offered a barren interval between
1030–801 m depth with one exception at 870 m (103 speci-
mens). The samples at 780 m and 760 m were very poor in
nannofossils (<5 specimens). In the well of Laa 1, all samples
between 1840–1360 m depth except one at 1630 m (3 speci-
mens) were barren while underlying and overlying samples
contained partly numerous specimens. Finally, in the well of
Wildendürnbach, all samples below 1055 m except one sam-
ple at 1254.3 m (307 specimens) proved to be barren.
The samples investigated for dinoflagellate cysts were
barren or offered a strongly reduced amount of specimens
(Appendix E) in the same intervals as the calcareous nanno-
fossils were impoverished. In the well of Schaubing, all inves-
tigated samples between 131–65 m depth contained
dino flagellate cysts. However, while all samples below 80 m
contained more than 100 specimens, the two uppermost
samples contained only sparse specimens (At 72 m depth 26
specimens, at 65 m depth, only 10 specimens).
In the well of Streithofen 1, all samples contained less than
100 specimens. While all samples below 990 m contained
between 6 to 74 dinoflagellate cysts, most samples above
965 m depth are barren. Only the uppermost three samples
(249.3 m, 151.5 m, 53.8 m) contained a very low amount of
two to seven specimens.
In the well of Wildendürnbach, all samples between
1533–1301 m were barren while the lowermost sample at
1563 m and 8 of 10 samples between 1254.5–753 m contained
dinoflagellate cysts. The samples between 1155–1051 m
offered only very few (>12) dinoflagellate cysts.
Mineralogy
The investigated samples consist of varying amounts of
quartz, K-feldspar, plagioclase, calcite, dolomite, muscovite,
chlorite and pyrite. Kaolinite, halite, gypsum and glauconite
were detected in several samples. Carbonate contents
(weight %) range between <5–40 % with few outliers of
carbonate-cemented sands. As the primary carbonate content
is the matter of interest here, diagenetically carbonate-cemen-
ted sands were excluded from the profiles or they are ignored
in the interpretation. Clay mineralogy analysis indicate
varying amounts of smectite, illite, chlorite and kaolinite.
Discussion
Calcite Minimum Interval
Depth profiles of carbonate content, XRD peak heights of
calcite and pyrite and XRF cps of Ca (Figs. 5–12) indicate
a prominent, up to 800 m thick interval within the pelites of
the investigated profiles. While carbonate contents range
between 15–25 % below and above, they fall mostly below
12 % within this interval. It must be taken into account that
Carbonate Bomb measurements become very inaccurate below
15 % and tend to overestimate carbonate contents at very low
levels. This may partly obscure the decrease. The reduced
Fig. 3. The sedimentary log of Wildendürnbach K4 between
1355–1351 m is presented as a facies example for the analysed drill
cores of the Wildendürnbach Fm. Drill core intervals comprised
1–5 m with gaps of 40–250 m in between. Pelitic deposits interrupted
by turbiditic fining upward cycles or other mass movements such as
mudflows are common.
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Fig. 4. Calcareous nannofossils from the investigated boreholes. The microphotographs are taken under Cross-Polarized Light (XPL) and
Bright Field (BF): 1 — Coccolithus pelagicus (coccosphere, XPL, sample POR-2/437); 2 — Reticulofenestra pseudoumbilicus (XPL, sample
POR-2/552); 3 — Reticulofenestra pseudoumbilicus (XPL, sample POR-2/1254); 4 — Reticulofenestra gelida (XPL, sample POR-2/1254);
5 — Helicosphaera ampliaperta (>10 µm, XPL, sample POR-2/552); 6 — Helicosphaera ampliaperta (<10 µm, XPL, sample POR-2/552);
7 — Helicosphaera ampliaperta (>10 µm, XPL, sample WDK-4/752); 8 — Helicosphaera scissura (XPL, sample WDK-4/752);
9 — Helicosphaera mediterranea (XPL, sample POR-2/1254); 10 — Helicosphaera carteri (XPL, sample POR-2/1254); 11 — Helicosphaera
carteri (XPL, sample WDK-4/854.5); 12 — Braarudosphaera bigelowii (XPL, sample WDK-4/752); 13 — Pontosphaera multipora (XPL,
sample WDK-4/752); 14 — Cyclicargolithus floridanus (XPL, samples STRTH-1/964.8); 15 — Reticulofenestra haqii (XPL, samples STRTH-
1/1022.6); 16 — Coronosphaera mediterranea (XPL, sample WDK-4/752); 17 — Syracosphaera cf. pulchra (XPL, sample POR-2/554.4);
18 — Syracosphaera? cf. oneillii (XPL, sample POR-2/552); 19 — Sphenolithus moriformis (XPL, sample WDK-4/854.5); 20 — Reticulofenestra
minuta (XPL, sample POR-2/1254).
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Fig. 5. Depth profiles of the well of Schaubing: Counted specimens of calcareous nannofossils, carbonate content (weight %), the characteristic
XRD peak-heights for calcite and pyrite, the cps for Ca and the smectite / illite ratio are plotted against drill-core depth. Drill-core positions are
shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset of the Calcite Minimum Interval (CMI).
The calcite-cemented sample at 24 m depth was excluded from interpretation. XRD netto (peak height − background) peak height for calcite:
3.03 Å; for pyrite: 2.70 Å.
Fig. 6. Depth profiles of all samples (including pelites and sands) of the well of Streithofen 1: Absence / Presence of calcareous nannofossils,
carbonate content (weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca are plotted against drill-core depth.
Drill-core positions are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset of the Calcite Minimum
Interval (CMI). XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
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carbonate contents correlate with strongly reduced XRD peak
heights of calcite. The nannofossil investigations indicate that
the strongly reduced calcite content intervals are consistent
with the absence of primary and reworked calcareous nanno-
fossils while nannofossils occurred below and above this
interval. The onset of this interval is also characterized by
increasing pyrite peak heights, immediately followed by
the overall decrease of pyrite below detectable amounts.
XRF-data of Ca (presented as cps/depth) constitute an addi-
tional proxy. Hereinafter, we define the interval of reduced
calcite content as a significant event, the Calcite Minimum
Interval (CMI).
Particularly, the depth-profiles of Schaubing (Fig. 5) record
a strong and sharp decrease of calcite contents around 80 m.
Pyrite also decreases and shows strongly varying values
between 80–50 m. While all samples below 80 m revealed
a rich nannofossil flora and numerous individuals, the samples
were (nearly) barren above 80 m. The samples at 72 m and
65.4 m contained only few individuals.
The profile of Streithofen 1 (Figs. 6–7) indicates the onset
of the CMI between 850 m and 800 m. Although the CMI can
be identified if all samples are plotted (Fig. 6), the CMI
becomes more obvious if only pelitic samples are taken into
account (Fig. 7).
Altough the profile of Altenmarkt T1 offered only few drill
cores (Figs. 8–9), the pelites (Fig. 8) indicates reduced calcite
contents between 1000–800 m. The profile of cuttings (Fig. 9)
reveals the onset of the CMI around 1125 m followed by
a pyrite peak at 1100 m and a drop of pyrite values below
detection limits above 1050 m. Pyrite was detected in all sam-
ples above 900 m. The calcite content recovers between
1000 m and 900 m. Calcareous nannofossils were absent in all
but two samples between 1125 m and 800 m and present in all
remaining samples.
Pelitic samples of the two drill cores of Laa (1799–1794 m,
1638–1632 m) record reduced calcite contents and are barren
of calcareous nannofossils. Cuttings from every 20–40 m
(samples between 1630 m and 1470 m were excluded due to
contamination) indicate the onset of the CMI around 1850 m.
The pyrite values slightly increase to a maximum at 1840 m
and drop below detection limit at 1820 m. The pyrite reappears
at 1450 m. Calcareous nannofossils are absent in all except
one sample between 1850–1340 m and present in all samples
above and below.
The profile of Wildendürnbach (Fig. 11) offers large varia-
tions of calcite and Ca values which were caused by the sam-
pling method. Samples of all lithologies were taken for every
1 m of available drill core. Therefore, rare lithologies such
as carbonate-cemented sands appear overrepresented, while
the domi nating carbonate-poor pelitic lithology is underesti-
mated. Further on, varying drill core diameters indicate, that
drill cores of other wells were mixed with drill cores of
Wildendürnbach K4. Nevertheless, the onset of the CMI can
be identified around 1530 m. A corrected profile, where sands,
muds, drill gouges and (according to the drill core diameter)
suspicious samples were excluded, reveals the CMI more
clearly at 1530 m (Fig. 12). After the onset of the CMI,
the pyrite contents increase to a maximum at 1530 m and
decrease below detection limit at 1450 m. Pyrite reappears at
1250 m. The calcite content recovers with strong fluctuations
between 1300 m and 1100 m. All except one sample below
1050 m were barren of microfossils while all samples above
1050 m contained nannofossils.
Clay mineral investigations indicate increased smectite /
illite ratios within the CMI. Smectite/illite ratios double from
1 to 2 in the well of Schaubing (Fig. 5). In the well of
Wildendürnbach K4, smectite/illite ratios reach values up to 3
for several samples. For the well of Streithofen 1, the increase
is less obvious, but while most samples underlying the CMI
show smectite/illite values clearly below 1, samples of the CMI
show ratios around or clearly above 1.
In general, carbonate, calcite, and Ca contents provide good
proxies for the CMI which is characterized by the absence of
both autochthonous and reworked calcareous nannofossils,
dinoflagellate cysts (unpublished data, this study), reduced
pyrite contents and usually increased smectite / illite ratios. We
define the onset of the CMI by the drop in calcite and the dis-
appearance of primary and reworked calcareous nannofossils.
The upper limit of the CMI is represented by a more broad
transitional recovery zone than a sharp boundary. The slow
and discontinuous increase of calcite contents in the upper part
of the CMI and the sporadic occurrence of calcareous nanno-
fossils within the CMI complicate a precise definition of
the upper boundary. All attempted precise definitions (reap-
pearance of nannofossils, increase of calcite or pyrite contents)
delivered conflicts and uncertainties.
Micropaleontology and biostratigraphy
The investigated sediments belong to the broad interval from
upper NN2 — Discoaster druggii Zone to NN4 —Helico
sphaera ampliaperta Zone (Martini 1971). Using the standard
zonation of Okada & Bukry (1980) this correlates to the CN2
— Sphenolithus belemnos Zone and the CN3 — Helicosphaera
ampliaperta Zone.
The Early Miocene nannoplankton biostratigraphy (NN2–
NN4 interval) is based on the presence of several species, such
as Discoaster druggii, Sphenolithus disbelemnos, S. belemnos,
S. heteromorphus, Triquetrorhabdulus carinatus and Helico
sphaera ampliaperta (Martini 1971). In the investigated
samples the only primary markers present are Helicosphaera
ampliaperta and Sphenolithus heteromorphus.
Helicosphaera ampliaperta is abundant in the upper part of
the Wildendürnbach K4 (sample WDK-4/752) and a drastic
decrease is noticed downward. H. ampliaperta is present but
very rare in the Schaubing, in Laa 1, Altenmarkt-T1 and in
Streithofen 1 boreholes.
The marker Sphenolithus belemnos (restricted to NN3) is
completely missing, while Sphenolithus heteromorphus
(NN3/NN4 – top NN5) is present in only one sample from
the Wildendürnbach K4 borehole (WDK-4/854.5) above
the CMI (Appendix C, Wildendürnbach K4).
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Fig. 7. Depth profiles of pelitic samples of the well of Streithofen 1: Absence / Presence of calcareous nannofossils, carbonate content
(weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca are plotted against drill-core depth. Drill-core
positions are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset of the Calcite Minimum Interval
(CMI). XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
Fig. 8. Depth profiles of pelitic drill core samples of the well of Altenmarkt i. T. 1: Absence / Presence of calcareous nannofossils, carbonate
content (weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca plotted against drill-core depth. Drill-core
positions are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset and termination of the Calcite
Minimum Interval (CMI). XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
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Although very rare, the presence of other species is some-
how supportive for the biostratigraphy assignment. The spe-
cies Sphenolithus conicus appears in sample WDK-4/905(2)
below the samples containing S. heteromorphus. Another
species restricted to the NN3-NN4 interval is S. multispinatus
which is very scarce and is present only in sample ALT-
T1/ 751.5(1) above the CMI (Appendix C, Altenmarkt T1).
The species Helicosphaera scissura, known to have an ear-
lier occurrence in the Central Paratethys (in NN2) is also very
rare, but present in some samples from Wildendürnbach K4,
Schaubing, Laa 1 and Altenmarkt T1 and is missing in
Streithofen 1 borehole.
The attribution to the above mentioned nannofossils stan-
dard zones from upper NN2 to NN4 would indicate in general
an interval from late Eggenburgian to early Badenian, in
the Central Paratethys regional stratigraphy (Piller et al. 2007;
Gradstein et al. 2012). No further reliable biostratigraphic sub-
division can be made due to the extreme rarity and nearly total
absence of some of the mentioned marker species. A largely
similar conclusion on biostratigraphy was given by Ćorić &
Roegl (2004) for the nearby Roggendorf-1 borehole, where
the carbonate-poor interval was dated as NN3 to lower NN4
based on nannofossil and foraminifera from under- and over-
lying sediments.
CMI Processes and causes
The reduced calcite content of the CMI can be ascribed to
one or several of the following causes and processes:
1. The overall calcite content, controlled by primary marine
production may be strongly reduced by an unfavorable
environment such as brackish water incursion (which is
supported by mollusc data of Mandic & Ćorić 2007) that
caused a breakdown of the primary (calcite and organ-
ic-walled) marine plankton productivity (Melinte 2004;
Mattioli et al. 2009; Hofer et al. 2011, 2013).
2. Calcite (both of primary production and detrital input)
was dissolved as a result of acidification of the water col-
umn (Zachos et al. 2005; Bordiga et al. 2013; Cobianchi
et al. 2015).
3. Calcite was dissolved after sedimentation by early dia-
genesis (Wilson & Thomson 1998; Wendler et al. 2002;
Jourabchi 2007).
4. Calcite was dissolved by a late diagenetic process, i.e.
pore water chemistry was already independent from open
water chemistry (Baumann et al. 2016).
5. The calcite content was strongly reduced by the dilution
due to increased clastic input rates (Haq 1991; Ricken
1996; Dunbar & Dickens 2003).
Cause 1, an environmental crisis (e.g., reduced salinities,
Hofer et al. 2011; Hofer et al. 2013) causing breakdown of
primary production, is indicated by the absence of micro- and
nannofossils. Especially the absence of dinoflagellate cysts,
which should be unaffected by calcite dissolution, speaks for
unfavorable primary conditions. Our data indicates a corre-
lation between nannofossil content and calcite content.
A breakdown of primary production of calcite may cause
reduced calcite contents. On the other hand, a breakdown of
primary production should not affect the redeposition of
reworked Mesozoic and Paleogene calcareous nannofossils.
The absence of such “allochthonous” calcareous nannofossils,
which constitute up to 50 % of the nannofossil assemblage
below and above the CMI, indicate, in addition, calcite disso-
lution and therefore cause 2, 3 or 4.
Cause 2 and 3, dissolution of calcite within the water column
(Zachos et al. 2005; Cobianchi et al. 2015) or during early
diagenesis in the sediment under near surface conditions
(Wilson & Thomson 1998; Jourabchi 2007), cannot be distin-
guished with the data at hand. It is hard to decide whether
the calcite was completely dissolved already in the water
column and never reached the floor, or if the dissolution
continued after deposition in pore spaces due to a changing
chemical composition of pore waters (which are still influen-
ced by the open water chemistry). Nevertheless, both models
explain the dissolution of calcite by a changed water chemistry
within that time-period. Our data suggests a relation between
the smectite / illite ratio and the calcite dissolution. Either,
the clay mineral composition influenced the pore-water or
water-column chemistry (or both) or external controlling
factors (such as volcanic ash input, e.g., Roetzel et al. 2014;
Cobianchi et al. 2015; Self et al. 2015) influenced both, water
chemistry and clay mineral composition.
Cause 4, late diagenetic processes, may have played a role
in further reducing the carbonate content and carbonate redis-
tribution as calcite concretions (Baumann et al. 2016). Never-
theless, the CMI seems to be bound rather to a certain
stratigraphic level than to a certain depth (CMI at surface in
the south and in 1000 m well depth in the north). The strati-
graphic succession of signals is always the same (i.e. sharp
decrease of calcite and disappearance of microfossils followed
by the disappearance of pyrite and a broad transition zone as
upper limit) arguing for a distinct time sequence of primary
controlling factors. Further on, the CMI is independent of
grain size, and appears both in sands to south and pelites to
north, respectively. In case of a purely diagenetic origin of
the CMI, we would rather expect a more heterogeneous signal
which is bound to a certain depth, lithology/grain size or mine-
ralogical composition.
Cause 5, dilution effect by increased clastic input (Haq
1991; Ricken 1996; Dunbar & Dickens 2003) seems unlikely,
as the CMI occurs both in massive sands in the south
(Schaubing, Streithofen 1) and in pelitic sediments to the north
(Wildendürnbach K4, Laa 1). Further on, the data indicate,
that the calcite contents of sands are usually higher than of
the pelites within the CMI. In addition, dilution would not
explain the absence of calcareous nannofossils and dinofla-
gellate cysts. Therefore dilution (cause 5) is excluded.
For these reasons, a combination of cause 1 (environmental
crises), 2 (calcite dissolution in the water column) and 3
(calcite dissolution in the near surface pore waters) is pre-
ferred to explain the CMI. A change in the water column (and
associated near-surface pore-water) chemistry that resulted in
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Fig. 9. Depth profiles of all cutting samples of the well of Altenmarkt i. T. 1: Absence / Presence of calcareous nannofossils, carbonate content
(weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca plotted against drill-core depth. Drill-core positions
are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset and termination of the Calcite Minimum
Interval (CMI). XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
Fig. 10. Depth profiles of all cutting samples of the well of Laa 1: Absence / Presence of calcareous nannofossils, carbonate content (weight %),
the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca plotted against drill-core depth. Drill-core positions are shown by
the black intervals of the inserted drill-core profile. Dashed lines indicate the onset of the Calcite Minimum Interval (CMI) as well as the limits
of the “Transition Zone” which constitutes the upper limit of the CMI. Samples between 1640–1460 m were contaminated and therefore
excluded. XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
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an acidification caused a primary dissolution of calcite and
(to a much lower degree) of dolomite. The primary production
was severely constrained or completely ceased. The reduction
of organic sulfur controlled the pyrite content. At the onset of
the crises, more organic material was available and therefore,
the pyrite contents temporarily increased. The permanent
absence of primary production caused a fast, but compared to
calcite delayed decrease in pyrite.
Paleogeographic and tectonic interpretation
The CMI comprises the upper Ottnangian Traisen Fm.
which constitute already identified deposits of the Rzehakia
Lake System (formerly Rzehakia or Oncophora Beds, e.g.,
Mandic & Ćorić 2007; Gebhardt et al. 2013). Therefore,
the CMI and the Wildendürnbach Fm. in the basinal part of
the LAMB correlate to the upper Ottnangian and their deposi-
tion can be linked to the Rzehakia Lake System (Harzhauser &
Mandic 2008).
Thus, we conclude that the CMI was caused by the late
Ottnangian regression which initiated the establishment of
brackish-water environments collectively termed as Rzehakia
Lake System, interpreted as marine-derived brackish lakes
(Čtyroký 1968; Harzhauser & Mandic 2008). This corre-
sponds to the mid-Burdigalian sea-level lowstand Bur4 (Piller
et al. 2007; Krijgsman & Piller 2012). During that sea-level
lowstand, huge amounts of sediments were delivered from
the Alpine orogen. This can be seen at Streithofen 1 (Figs. 6,
7, 13), where due to locally high tectonically driven subsidence
rates more than 800 m of sediments were deposited within the
CMI probably in less than 0.5 Ma (Krijgsman & Piller 2012).
The combination of the high sedimentation rates, tectonic
processes and the sea-level lowstand caused the closure of
the gateway at the Amstetten Swell between the western and
eastern Austrian Molasse Basin (e.g., Roegl & Steininger
1983; Bieg 2005; Harzhauser & Mandic 2008; Sant et al.
2017b) and isolated the upper Austrian and Bavarian Molasse
Basin. This closure in combination with the progressing nar-
rowing of the LAMB by the advancing Alpine and Carpathian
fold-thrust belt east of the Bohemian Massif (Ustaszewski et
al. 2008; Beidinger & Decker 2014), may have led to a (semi-)
isolated water body in the LAMB and to a change from well
circulated open- marine (Faupl & Roetzel 1987; Bieg 2005;
Roetzel et al. 2006; Grunert et al. 2010b) to restricted and less
circulated to stagnant water column (Harzhauser & Mandic
2008). This is supported by the work of Mandic & Ćorić
(2007) who describe an upper Ottnangian brackish mollusc
assemblage within the Traisen Fm.
In addition, the increased smectite contents indicate
enhanced input of volcanic ashes from northern Hungary and
southern Slovakia (Nehyba & Roetzel 1999; Roetzel et al.
2014), which probably had influence on the water chemistry
and increased acidity (Jones & Gislason 2008; Duggen et al.
2010; Ayris & Delmelle 2012; Self et al. 2015). The isolation
of the LAMB was terminated by the Karpatian transgression
(Piller et al. 2007; Roetzel et al. 2009; Grunert et al. 2010a)
after the Bur4 lowstand, beginning at c. 17.2 Ma (Krijgsman
& Piller 2012; Sant et al. 2017b).
Stratigraphic and paleogeographic implications
Numerous, mostly poorly defined lithostratigraphic terms
such as Oncophora Beds, Rzehakia Beds, Lužice Fm, “Sand -
s treifenschlier”, “Haller Schlier”, “Jüngerer Schlier”, have been
used for Ottnangian deposits mostly in the Austrian part of the
NAF (Čtyroký 1972; Aniwandter et al. 1990; Roegl et al. 1997;
Sauer & Kuffner 1997; Roetzel et al. 1999a; Kuffner 2001;
Kováč et al. 2004; Gebhardt et al. 2013; Wimmer-Frey et al.
2013). Recently, Pippèrr et al. (2018) formalized the Onco-
phora Fm. in SE Germany (Bavaria) and Upper Austria.
The identification of the CMI as a litho- and chemostratigraphic
marker may provide an appropriate instrument for a refined
and simplified lithostratigraphic concept of Ottnangian sedi-
ments in the LAMB (Fig. 14). Although the CMI can be recog-
nized in sands, pelites should be preferred for tracing it.
We propose to define the boundary between “Robulus
Schlier” and Traisen Fm. by the onset of the CMI. Furthermore,
the termination of the CMI can be used to define the boundary
between the upper Ottnangian Traisen Fm. and the overlying
Karpatian Laa Fm. Several descriptions of the Zellerndorf Fm.
indicate the existence of a CMI-like decalcified interval
(Roetzel et al. 1999a, c, 2006, 2014; Grunert et al. 2010b).
Nevertheless, discussion is ongoing whether this interval con-
stitutes the upper Ottnangian part of the Zellerndorf Fm.
(Reinhard Roetzel per. comm. 2017).
To avoid confusion by the usage of a significantly emended
and redefined Zellerndorf Fm., we introduce the term Wilden-
dürnbach Fm. which constitutes the deposition of the central
basinal parts of the Rzehakia Lake System in the LAMB and
define its limits by the CMI (Appendix A).
In our stratigraphic model (Fig. 14, column “LAMB, This
Study”), the Zellerndorf Fm. represents the proximal pelitic
Ottnangian deposits as defined at outcrops along the eastern
margin of the Bohemian Massif. The calcareous lower part
correlates to the basinal “Robulus Schlier s.l.” and the decalci-
fied upper part may represent the CMI and correlates at least
partly to the Wildendürnbach Fm. and the Traisen Fm. We
propose to delimit the Zellerndorf Fm. by its facies, minera-
logy and depositional environment. The Zellerndorf Fm.
there fore comprises non-turbiditic deposits derived from the
Bohe mian Massif while turbiditic sands of the Wilden dürn bach
Fm. were derived from the Alpine and Carpathian orogen.
Further on, we propose to define the upper boundary of the
Zellern dorf Fm. by the termination of the CMI. Whether the
Zellerndorf Fm. should be divided into a lower/middle Ottnan-
gian marine unit and an upper Ottnangian predominantly
brackish unit remains open and needs more investigations.
Correlation throughout the NAFB
The CMI constitutes an effective tool for a correlation of
the autochthonous Lower Austrian Molasse to the upthrusted
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Fig. 11. Depth profiles of all samples of the well of Wildendürnbach K4: Absence / Presence of calcareous nannofossils, carbonate content
(weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca plotted against drill-core depth. Drill-core positions
are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset of the Calcite Minimum Interval (CMI). XRD
netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
Fig. 12. Depth profiles of pelitic samples of the well of Wildendürnbach K4: Absence / Presence of calcareous nannofossils, carbonate content
(weight %), the characteristic XRD peak-heights for calcite and pyrite and the cps for Ca plotted against drill-core depth. Drill-core positions
are shown by the black intervals of the inserted drill-core profile. Dashed lines indicate the onset and termination of the Calcite Minimum
Interval (CMI). XRD netto (peak height − background) peak height for calcite: 3.03 Å; for pyrite: 2.70 Å.
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allochthonous Molasse in Lower Austria and in the Czech
Republic. Krhovský et al. (2001) related the Austrian
“Waschberg Unit s.l.” (including the “Roseldorf Zone” and
the “Waschberg Unit s. str.”, Fig. 1) to the Czech Pouzdřany
and Ždánice Units. The Ždánice Unit constitutes the conti-
nuation of the Waschberg Unit in the Czech Republic with
tectonic slices, the Pouzdřany Unit, at its front. Grill (1962)
already correlated the generally micro- and nannofossil-
barren non-calcareous “clays and limonitic claystones”
(“Eisenschüssige Tone und Sande”, Grill 1962) to the “Onco
phora Beds”. Gebhardt et al. (2013) also correlated the Traisen
Fm. to the “Eisenschüssige Tone und Sande”. Preliminary
field mapping results of the Austrian Geological Survey
(Holger Gebhardt per. comm. 2017) support the finding, that
these sediments represent the CMI in the upthrusted part of
the LAMB. Various authors described the “Eisenschüssige
Tone und Sande” as calcite-poor to -free and correlated them
to the Pavlovice Fm. of the Pouzdřany Unit and to the upper
part of the Křepice Fm. (Krhovský et al. 2001; Krenmayr et al.
2002; Roegl et al. 2009; Roetzel et al. 2009). The absence of
microfossils and calcite is mentioned for both the Pavlovice
and for the Křepice formations, respectively, which indicates
that the CMI probably comprises both units. This is in good
agreement with correlations to the “Eisenschüssige Tone und
Sande” of Grill (1962).
As the CMI represents the marker signal of the late
Ottnangian (Piller et al. 2007), we propose a slightly modified
stratigraphy of the allochthonous Molasse in Lower Austria and
the Czech Republic. In this model, the “Eisenschüssige Tone
und Sande”, the Pavlovice Fm. and the Křepice Fm. belong to
the late Ottnangian Rzehakia Lake System. Con sequently,
the underlying “Schiefrige Tonmergel”, the Sakvice Fm.
and the Boudky Fm. include the lower and middle Ottnangian.
The lower and upper boundaries of these units may thus
be uni formly defined by using the onset and termination of
the CMI.
Equivalent CMI-deposits in the area of the (later develo-
ping) Vienna Basin were not reported so far in published lite-
rature. According to the stratigraphic scheme of Kováč et al.
(2004), such an interval should comprise parts of the Lužice
Fm. and / or the Laksary Fm. However, a sedimentation gap has
been assumed for the late Ottnangian (Harzhauser & Mandic
2008; Reichenbacher et al. 2013; Sant et al. 2017b). Never-
theless, in the light of the identification and stratigraphic value
Fig. 13. Correlation of the CMI representing the upper Ottnangian over investigated wells. CMI comprises the Traisen Fm. and the Wilden-
dürnbach Fm. For Altenmarkt 1, Laa 1 and Wildendürnbach K4, the dashed line indicates the extent of the transitional zone between the upper
Ottnangian and the Karpatian (Laa Fm.).
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Fig. 14.
Stratigraphic
chart
comparing
the
proposed
stratigraphy
to
other
(modified
) stratigraphic
models
(Krhovský
et
al.
2001;
Kováč
et
al.
2004;
Piller
et
al.
2004;
Rupp
et
al.
2008;
Schneider
et
al.
201
1;
Sant
et
al.
2017a;
Pippèrr
et
al.
2018).
Calcareous
nannofossil
zones
were
taken
from
Martini
(1971)
and
cyclostratigraphy
was
taken
from
Hardenbol
et
al.
(1998).
The
chart
was
partly
prepared
using
the
“T
ime
Scale
Creator”
software
(Ogg
&
Lugowski
2017).
The
yellow
box
indicates
the
stratigraphic
units
af
fected
by
the
CMI.
The
blue
striped
pattern
indicates
hiatuses.
Ger
.
Mod.: Germany modified; Dan.: Danube;
W
.U.:
W
aschber
g Unit; s. str
.: senso stricto; s.l.: senso lato.
331
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
of the CMI in the NAFB, a careful revision may be appropriate
for correlative profiles in the Vienna Basin (e.g., Harzhauser et
al. 2018).
A correlation of the CMI to the west, to Upper Austria
and Bavaria is not straightforward and partly speculative.
As the onset of the CMI corresponds to a major paleogeo-
graphic re-organization with the closure of the seaway west of
the LAMB by the swell of Amstetten (Bieg 2005; Pippèrr &
Reichenbacher 2017; Sant et al. 2017a), the water bodies in
the LAMB and those of Upper Austria and Bavaria were at
least partly disconnected during the late Ottnangian (Bieg
2005; Mandic & Ćorić 2007; Harzhauser & Mandic 2008;
Kováč et al. 2017; Sant et al. 2017a, b). A direct correlation of
a signal such as the CMI, which was caused by changing water
chemistry is restricted to the basin and thus connected water-
bodies. Nevertheless, brackish conditions were also estab-
lished in western Austria and southern Germany (Rupp et al.
2008; Reichenbacher et al. 2013; Pippèrr & Reichenbacher
2017; Sant et al. 2017a, b) reflecting the global sea-level fall
of Bur4.
In Upper Austria and South Germany the subdivision
between the fully marine lower and the restricted marine
middle Ottnangian is better defined than in Lower Austria
(Wenger 1987; Rupp et al. 2008; Grunert et al. 2010a;
Schneider et al. 2011; Reichenbacher et al. 2013; Pippèrr &
Reichenbacher 2017; Sant et al. 2017a). In Upper Austria and
eastern Bavaria, the Rzehakia Lake System is represented by
the classical “Oncophora Beds” with the typical
Rzehakia
mollusc assemblage (Papp 1955; Papp et al. 1973; Rupp et al.
2008). Pippèrr et al. (2018) recently formalized these deposits
as Oncophora Fm. and stated, that only the lower Oncophora
Fm. is of Ottnangian age while the upper Oncophora Fm.
represents already Karpatian deposits. The Oncophora Fm.
overlies the “Glauconitsande und Blättermergel” in eastern
Bavaria and the “Robulus Schlier s. str.” and the Innviertel
Group in Upper Austria, which comprises lower and middle
Ottnangian units. Whether the upper Oncophora Fm. was
affected by the early Karpatian transgression or not is under
discussion (Lemcke 1988; Piller et al. 2007; Pippèrr &
Reichenbacher 2017).
In the remaining part of the S-German Molasse Basin,
the Upper Brackish Molasse (OBM for the German “Obere
Brackwassermolasse” to avoid confusion with the “Untere
Brackwassermolasse”) corresponds to the Rzehakia Lake
System. According to Pippèrr & Reichenbacher (2017) and
Sant et al. (2017a), the OBM comprises the upper Ottnangian
Grimmelfingen Fm. and the lower Karpatian Kirchberg Fm.
Where fossils are absent, Reichenbacher et al. (2013) distin-
guish the Grimmelfingen Fm. from the Kirchberg Fm. by
reduced carbonate contents. In the southwest-German Molasse
Basin, time equivalent units to the “Robulus Schlier s.l.” are
the lower Ottnangian “OMM-Basisschichten” and Kalkofen
Fm. and the middle Ottnangian Baltringen and Steinhöfen Fm.
(in Fig. 14 summarized as Upper Marine Molasse, Heckeberg
et al. 2010). The new model of Sant et al. (2017a) (model 2)
and of Pippèrr & Reichenbacher (2017) with an upper
Ottnangian, non-calcareous brackish Grimmelfingen Fm.
and a lower Karpatian Kirchberg Fm. representing the early
Karpatian transgression is in good agreement with our
model of the CMI (Traisen Fm. And Wildendürnbach Fm.)
terminated by the Bur4 transgression. However, this is specu-
lative as no comparable chemical data are known from
Bavaria.
Conclusions
Based on biostratigraphical, lithological and chemical depth
profiles of wells throughout the Lower Austrian Molasse
Basin (LAMB), we identify a prominent and stratigraphically
significant unit, the Calcite Minimum Interval (CMI) which
constitutes a lithological expression and chemical signal of
the Rzehakia Lake System (Harzhauser & Mandic 2008).
Consequently, this interval is of late Ottnangian age and
related to the mid-Burdigalian Bur4 sea-level lowstand (Piller
et al. 2007; Rupp et al. 2008; Sant et al. 2017a). The CMI
offers a valuable litho- and chemostratigraphic signal for
an interval of high sedimentation rates, poor biostratigraphical
resolution and extremely poor to lacking microfossil content.
We define the onset of the CMI as corresponding to the sharp
decrease of calcite contents and the disappearance of auto-
chthonous (and reworked) calcareous nannofossils. Further
on, we define the termination of the CMI by the permanent
increase of pyrite contents and the constant reappearance of
calcareous nannofossils, which correlates with a more diffuse
and gradational increase of calcite contents.
We propose a new stratigraphic model that correlates
the limits of the CMI to the middle/upper Ottnangian and
the Ottnangian / Karpatian boundary (Piller et al. 2007;
Harzhauser & Mandic 2008) and allows for a detailed correla-
tion of upper Ottnangian units. Further on, we introduce
the newly defined Wildendürnbach Fm. comprising the upper
Ottnangian depositions in the central, basinal parts of the LAMB
and define its limits by the CMI.
We discuss the capacity of the CMI as a litho- and chemo-
stratigraphical key horizon to correlate the late Ottnangian
time interval throughout eastern Austrian and Czech part of
the Molasse Basin. According to lithological descriptions
and former comparisons, we correlate the Traisen Fm.,
the Wildendürnbach Fm., the upper part of the Zellerndorf
Fm. and the “Eisenschüssige Tone und Sande” to the upper
Ottnangian (Roetzel et al. 1999a, 2014; Krhovský et al. 2001;
Krenmayr et al. 2002; Harzhauser & Mandic 2008; Gebhardt
et al. 2013). The Czech Křepice and Pavlovice Fm. should be
investigated in detail, whether they represent the continuation
of the CMI into the Czech Republic as already suggested
(Krhovský et al. 2001; Krenmayr et al. 2002; Roetzel et al.
2009). In the west, the Grimmelfingen Fm. in western Bavaria
may represent time equivalent deposits and the newly defined
Oncophora Fm. (Pippèrr et al. 2018) may constitute partly
time equivalent deposits in Upper Austrian and eastern
Bavaria.
332
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Acknowledgments: This work was funded by a cooperation
project of OMV Exploration and Production AG and the Uni-
versity of Vienna. The publication was approved by OMV.
We thank especially Holger Gebhardt, Stjepan Ćorić, Reinhard
Roetzel, Philipp Strauß, Thomas Kuffner, Wolfgang Hujer,
Mathias Harzhauser, Dörte Theobalt, Andreas Beidinger and
Kurt Decker for their assistance and numerous fruitful discus-
sions.
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GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Formal Definition of the Wildendürnbach Formation
Validity: Described in unpublished OMV drilling reports as
“Oncophora Beds” or “Fisch Fazies”. A sedimentological
description of the type section and reference profiles can be
found in unpublished oil company (OMV) reports by Kuffner
(2001), Sauer & Kuffner (1997) and Palzer-Khomenko et al.
(2016a).
Type area: Central parts of the Lower Austrian Molasse
Basin north of the Danube and southwestern Czech Molasse
Basin. The unit is only described from drill cores.
Type section: The well of Laa 1 (48°42’28” N, 16°25’48” E)
between 1550–1855 m depth represents the type section. Two
drill cores (1794–1799 m and 1632–1638 m), a self-potential
log, a resistivity log and cutting-samples every 20–40 m as
well as OMV-archive data (sedimentological descriptions,
heavy mineral data, paleontological data, lithostratigraphic
interpretation) are available. The section was investigated and
described by internal OMV-reports such as Kuffner (2001)
and Palzer-Khomenko et al. (2016a). Preliminary results were
also presented by Knierzinger et al. (2015), Palzer et al. (2015)
and Palzer-Khomenko et al. (2016b).
Reference section(s): Reference sections are the OMV-
wells of Wildendürnbach K4 (48°44’58” N, 16°30’51” E;
1300–1535 m depth) and Altenmarkt T1 (48°34’59” N,
16°14’03” E; 880–1125 m depth). Self-potential logs, cuttings
and OMV-archive data are available. For Wildendürnbach K4,
a resistivity log is available as well. The reference profiles
were investigated by the same studies as the type section.
Additionally, Wildendürnbach K4 was described more closely
by Sauer & Kuffner (1997). Kreutzer (1993) and Hamilton
(1997) described and discussed the subcrop stratigraphy
around Wildendürnbach K4.
Remarks: No surface outcrops apart from wells and drill
cores are known for the Wildendürnbach Formation. The drill
cores available are in parts of poor quality, especially in
the well of Wildendürnbach K4. According to the better drill
core quality, Laa 1 was chosen as type profile instead of
Wildendürnbach K4.
Derivation of name: After the reference well section
Wildendürnbach K4 well and the nearby village of
Wildendürnbach. The term Laa Formation already exists.
Synonyms: The “Fisch-Facies” frequently used in well
descriptions is more or less equivalent. Nevertheless, “Fisch-
Fazies” is a descriptive term which indicates pelitic and
semi-pelitic sediments rich in fish scales. Although fish scales
are a common feature for the Wildendürnbach Formation, they
are also found in other intervals. Vice versa, the Wildendürnbach
Formation includes layers free of fish scales.
Another synonym are the so called Oncophora Beds.
The term mostly describes calcite-poor and microfossil-free
sand- dominated sediments including pelitic intervals at
the base. Gebhardt et al. (2013) redefined the exposed
Oncophora Beds south of the Danube (mostly massive sands)
as Traisen Formation. The Traisen Formation represents
the southern, proximal coarse grained equivalent and continua-
tion of the (semi)-pelitic Wildendürnbach Formation. The term
“Oncophora Beds”, which was used for pelitic or turbiditic
intervals in the central basinal parts, can be seen as synonym
of the Wildendürnbach Formation. Around the village of
Wildendürnbach (48°45’20” N, 16°30’02” E) at the Czech
border, the term “Oncophora Beds” was used for a sand
domi nated, carbonate bearing interval including a marine
micro-fauna which is clearly overlying the calcite poor
Wilden dürnbach Formation (Aniwandter et al. 1990; Hamilton
1997). There, the term “Oncophora Beds” is synonymous for
Laa Formation.
The (especially in older literature) frequently used term
“Sandstreifenschlier” (Piller et al. 2004) includes pelitic and
semi-pelitic Ottnangian sediments. It is equivalent to the
Wilden dürnbach Formation, the lower pelitic part of the
Traisen Formation and the (in Lower Austria also poorly
defined) “Robulus Schlier sensu lato”.
The Zellerndorf Formation represents a not fully formalized
Ottnangian unit cropping out at the rim of the Bohemian
Massif between Maissau (48°34’13” N, 15°49’35” E) and the
Czech border (Roetzel et al. 1999; Roetzel et al. 2006; Roetzel
et al. 2015). In the Austrian Stratigraphic Chart of Piller et al.
(2004), it represents the deposits of the Ottnangian Molasse
Basin north of the Danube. The Zellerndorf Formation con-
sists of pelitic sediments and includes a calcareous interval
with a marine micro-fauna and a carbonate and micro-fossil
free, smectite rich interval (Roetzel et al. 2015). This calcite-
free interval of the Zellerndorf Formation represents the proxi-
mal continuation of the Wildendürnbach Formation. Despite
the fact that the Zellerndorf Formation represents the Ottnan-
gian sediments north of the Danube in the Austrian Strati-
graphic Chart, the term was usually not used in well-profile
descriptions and its usage was restricted to proximal outcrops
close to the Bohemian Massif. Nevertheless, the Wilden-
dürnbach Formation should replace the upper Ottnangian
non-calcareous part of the Zellerndorf Formation in the centre
of the Lower Austrian Molasse Basin.
Lithology: The Wildendürnbach Formation consists of
bluish-grey fine grained silts and silty clays with intercalated
unstructured coarse grained silts, muds and fine grained sands
as well as fining upward cycles of grey to yellowish sands and
yellowish to brownish muds. Beds of medium grained sands
SUPPLEMENT
Appendix A
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, 2018, 69, 4, 315–334
appear. Rip-up clasts of clay and mud usually occur at the ero-
sive base of the fining upward cycles. The sedimentary struc-
tures of sand-layers grade with decreasing grain size from
massive to planar parallel stratification, ripple cross lamina-
tion and mm laminated silts. Slumping structures frequently
occur. Dewatering-structures can be found. The pelites are
usually mica-rich and calcite-free. Intercalated sands consist
of quartz, muscovite, chlorite, dolomite and feldspar and show
a varying calcite content. Heavy mineral assemblages are
dominated by garnet and epidote/zoisite and contain low
amounts of zircon, rutile, tourmaline, titanite and amphibole
(Knierzinger et al. 2015). Carbonate Bomb (Mueller &
Gastner 1971) measurements confirm reduced carbonate
contents (<15 %; often <10 %) for the pelites. XRD analyses
reveal reduced calcite contents, an increased smectite/illite
ratio compared to under- and overlying units and the absence
of detectable amounts of pyrite.
Fossils: The Wildendürnbach Formation is usually free of
microfossils including the absence of re-sedimented Creta-
ceous and Paleogene nannofossils, which are common in over-
and underlying units. Where calcareous nannofossils are
present, they consist of the same assemblage as the underlying
Robulus Schlier and the overlying Laa Formation. A biostrati-
graphic distinction between Ottnangian and Karpatian is not
possible. Fish scales frequently occur, shell fragments are rare.
Plant remains usually occur in fining upwards cycles.
Origin, facies: Kuffner (2001) describes Tab, Tabc and Tbc
Bouma sequences for the drill cores of Laa 1. For
Wildendürnbach K4, Kuffner (2001) describes hemipelagic,
mudy and turbiditic sedimentation between 1300–1530 m.
Palzer-Khomenko et al. (2016a) follows the facies interpreta-
tion of Hamilton (1997) and Kuffner (2001) as a deeper-water
trough with turbiditic flow and other types of mass flows such
as slumps.
Chronostratigraphic age: late Ottnangian.
The Wildendürnbach Formation is interpreted to represent
the depositions in the centre of the Lower Austrian Molasse
Basin during the late Ottnangian Rzehakia Lake System
(Harzhauser & Mandic 2008). Piller et al. (2007) describes
the Ottnangian as a “strictly twofold stage with a normal
marine development in its lower part and a predominance of
restricted marine to fresh water environments in its upper
part”. Therefore the Wildendürnbach Formation corresponds
to the late Ottnangian sensu Piller et al. (2007).
Biostratigraphy: Microfossils are rarely found. Where
available, calcareous nannofossils are similar to underlying
and overlying units and indicate NN3-NN4.
Thickness: up to 300m (well of Laa 1).
Lithostratigraphically higher rank unit: Pixendorf Group
(includes then Dietersdorf Formation, Traisen Formation and
Wildendürnbach Fromation).
Lithostratigraphic subdivision: not yet defined.
Lower and upper boundary: The base and top of
the Wilden dürnbach Formation is principally defined by
the overall reduction in the carbonate content (the carbonate
minimum interval), i.e. the lower boundary by a relatively
sharp reduction in the carbonate content to almost zero (except
diagenetic carbonate redistribution and accumulation).
The upper boundary is often transitional over tens of metres
with a more gradual increase in carbonate content of pelites.
A more distinct upper boundary of the W.F. and thus lower
boundary of the Laa Formation (see also Rögl et al. 1997) can
be defined by the appearance of calcareous nannofossils (in
smear slides) and also pyrite, both typical for re-established
fully marine conditions, and (although not in detail investi-
gated in our study) the coeval appearance of a Karpatian
foraminiferal assemblage (Rögl et al. 1997; Ćorić & Rögl
2004).
Underlying units: Robulus Schlier s.l., Zellerndorf
Formation, “Sandstreifen Schlier”.
Overlying units: Laa Formation.
Lateral boundary: The Wildendürnbach Formation com-
prises the central basinal depositions of late Ottnangian age.
It is characterized by continuous pelitic deposition and pelites
interrupted by gradated sand layers with ripples and planar
parallel stratification of Alpine and Carpathian provenance
indicated by garnet-dominated heavy mineral spectras.
Lateral units: To the Bohemian Massif: Zellerndorf For-
mation; to the Alpine–Carpathian Orogen: Traisen Formation
and “Eisenschüssige Tone und Sande”; to the autochthonous
Czech Molasse Basin: unknown; to the allochthonous Zdanice
Unit: Pavlovice Formation.
Geographic distribution: Central parts of the Lower
Austrian and Czech Molasse Basin, from the area of Schaubing
to Wildendürnbach near the Czech border. Continuation into
the Czech Molasse Basin unknown.
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List of Calcareous Nannofossils
Cenozoic calcareous nannofossils:
Acanthoica sp.
Braarudosphaera bigelowii (Gran and Braarud 1935) Deflandre 1947
Calcidiscus leptoporus (Murray & Blackman 1898) Loeblich &
Tappan 1978
Calcidiscus pataecus (Gartner 1967) de Kaenel & Villa 1996
Calciosolenia fossilis (Deflandre in Deflandre & Fert 1954) Bown in
Kennedy et al. 2000
Coccolithus miopelagicus Bukry 1971
Coccolithus pelagicus (Wallich 1871) Schiller 1930
Coccolithus sp.
Coronocyclus baileyi da Gama & Varol 2013
Coronocyclus cf. nitescens Hay Mohler & Wade 1966
Coronosphaera mediterranea (Lohmann 1902) Gaarder 1977
Cyclicargolithus floridanus (Roth & Hay 1967) Bukry 1971
Discoaster deflandrei Bramlette & Riedel 1954
Discoaster cf. druggii Bramlette & Wilcoxon 1967
Discoaster sp.
Hayaster sp.
Hayella challengeri (Muller 1974) Theodoridis 1984
Helicosphaera ampliaperta Bramlette & Wilcoxon 1967
Helicosphaera carteri (Wallich 1877) Kamptner 1954
Helicosphaera euphratis Haq 1966
Helicosphaera intermedia Martini 1965
Helicosphaera mediterranea Muller 1981
Helicosphaera scissura Miller 1981
Helicosphaera vedderi Bukry 1981
Helicosphaera sp.
Hughesius tasmaniae (Edwards & Perch-Nielsen 1975) de Kaenel &
Villa 1996
Lithostromation sp.
Pontosphaera multipora (Kamptner 1948) Roth 1970
Reticulofenestra ampliumbilicus Theodoridis 1984
Reticulofenestra gelida (Geitzenauer 1972) Backman 1978
Reticulofenestra haqii Backman 1978
Reticulofenestra minuta Roth 1970
Reticulofenestra pseudoumbilicus (Gartner 1967) Gartner 1969
Sphenolithus conicus Bukry 1971
Sphenolithus heteromorphus Deflandre 1953
Sphenolithus moriformis (Brönnimann & Stradner 1960) Bramlette &
Wilcoxon 1967
Sphenolithus multispinatus Maiorano & Monechi 1997
Sphenolithus sp.
Syracosphaera cf. pulchra Lohmann 1902
Syracosphaera tanzanensis Bown 2005
Syracosphaera? cf. oneillii da Gama & Varol 2013
Syracosphaera sp.
Thoracosphaera sp.
Triquetrorhabdulus sp.
Umbilicosphaera jafari Müller 1974
Umbilicosphaera rotula (Kamptner 1956) Varol 1982
Reworked Cenozoic calcareous nannofossils:
Campylosphaera eroskayi (Varol 1989) Bown 2005
Campylosphaera sp.
Chiasmolithus cf. bidens (Bramlette & Sullivan 1961) Hay & Mohler
1967
Chiasmolithus cf. expansus (Bramlette & Sullivan 1961) Gartner 1970
Chiasmolithus sp.
Clausicoccus subdistichus (Roth & Hay in Hay et al. 1967) Prins
1979
Clausicoccus sp.
Coccolithus bownii Jiang & Wise 2007
Coccolithus foraminis Bown 2005
Coccolithus formosus (Kamptner 1963) Wise 1973
Coccolithus latus Bown 2005
Coccolithus pauxillus Bown 2005
Coccolithus staurion Bramlette & Sullivan 1961
Craticullithus sp.
Cruciplacolithus asymmetricus van Heck & Prins 1987
Cruciplacolithus tenuis (Stradner 1961) Hay & Mohler in Hay et al.
1967
Cruciplacolithus sp.
Cyclicargolithus luminis (Sullivan 1965) Bukry 1971
Discoaster barbadiensis Tan 1927
Discoaster cf. lodoensis Bramlette & Riedel 1954
Discoaster cf. nodifer (Bramlette & Riedel 1954) Bukry 1973
Discoaster sp.
Ericsonia robusta (Bramlette & Sullivan 1961) Edwards &
Perch-Nielsen 1975
Ericsonia staerkeri Bown 2005
Ericsonia subpertusa Hay & Mohler 1967
Ericsonia sp.
Helicosphaera recta (Haq 1966) Jafar & Martini 1975
Ilselithina fusa Roth 1970
Isthmolithus recurvus Deflandre in Deflandre & Fert 1954
Neochiastozygus sp.
Pontosphaera exilis (Bramlette & Sullivan 1961) Romein 1979
Pontosphaera sp.
Prinsius bisulcus (Stradner 1963) Hay & Mohler 1967
Prinsius martinii (Perch-Nielsen 1969) Haq 1971
Prinsius sp.
Reticulofenestra bisecta (Hay Mohler & Wade 1966) Roth 1970
Reticulofenestra daviesii (Haq 1968) Haq 1971
Reticulofenestra dictyoda (Deflandre in Deflandre & Fert 1954)
Stradner in Stradner & Edwards 1968
Reticulofenestra hillae Bukry & Percival 1971
Reticulofenestra lockeri Müller 1970
Reticulofenestra reticulata (Gartner & Smith 1967) Roth & Thierstein
1972
Reticulofenestra scrippsae Bukry & Percival 1971
Reticulofenestra stavensis (Levin & Joerger 1967) Varol 1989
Reticulofenestra umbilicus (Levin 1965) Martini & Ritzkowski 1968
Rhabdosphaera gracilentus (Bown & Dunkley Jones 2006) Dunkley
Jones et al. 2009
Sphenolithus acervus Bown 2005
Sphenolithus arthurii Bown 2005
Sphenolithus calyculus Bukry 1985
Sphenolithus ciperoensis Bramlette & Wilcoxon 1967
Sphenolithus distentus (Martini 1965) Bramlette & Wilcoxon 1967
Sphenolithus editus Perch-Nielsen in Perch-Nielsen et al. 1978
Sphenolithus pseudoradians Bramlette & Wilcoxon 1967
Sphenolithus radians Delfandre in Grassé 1952
Sphenolithus spiniger Bukry 1971
Toweius callosus Perch-Nielsen 1971
Toweius gammation (Bramlette & Sullivan 1961) Romein 1979
Toweius occultatus (Locker 1967) Perch-Nielsen 1971
Toweius pertusus (Sullivan 1965) Romein 1979
Appendix B
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THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
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Toweius rotundus Perch-Nielsen in Perch-Nielsen et al. 1978
Toweius selandianus Perch-Nielsen 1979
Toweius serotinus Bybell & Self-Trail 1995
Zygodiscus sp.
Zygrhablithus sp.
Mesozoic calcareous nannofossils:
Arkhangelskiella cymbiformis Vekshina 1959
Arkhangelskiella cf. maastrichtiensis Burnett 1997
Arkhangelskiella specillata Vekshina 1959
Arkhangelskiella sp.
Broinsonia enormis (Shumenko 1968) Manivit 1971
Broinsonia parca subsp. constricta Hattner et al. 1980
Calculites percernis Jeremiah 1996
Calculites obscurus (Deflandre 1959) Prins & Sissingh in Sissingh
1977
Calculites sp. Prins & Sissingh in Sissingh 1977
Chiastozygus sp.
Cretarhabdus sp.
Cribrosphaerella ehrenbergii (Arkhangelsky 1912) Deflandre in Piv-
eteau 1952
Cyclagelosphaera tubulata (Grün & Zweili 1980) Cooper 1987
Cyclagelosphaera sp.
Eiffellithus cf. eximius (Stover 1966) Perch-Nielsen 1968
Eiffellithus cf. gorkae Reinhardt 1965
Eiffellithus sp.
Gartnerago segmentatum (Stover 1966) Thierstein 1974
Lithraphidites bollii (Thierstein 1971) Thierstein 1973
Lithraphidites houghtonii Jeremiah 2001
Lucianorhabdus cf. maleformis Reinhardt 1966
Manivitella sp.
Micrantholithus hoschulzii (Reinhardt 1966) Thierstein 1971
Micrantholithus sp.
Microrhabdulus decoratus Deflandre 1959
Micula murus (Martini 1961) Bukry 1973
Micula premolisilvae Lees & Bown 2005
Micula prinsii Perch-Nielsen 1979
Micula staurophora Gardet 1955
Micula cf. swastica Stradner & Steinmetz 1984
Micula sp. Vekshina 1959
Nannoconus sp.
Parhabdolithus sp.
Prediscosphaera cretacea (Arkhangelsky 1912) Gartner 1968
Prediscosphaera spinosa (Bramlette & Martini 1964) Gartner 1968
Prediscosphaera sp.
Radiolithus planus Stover 1966
Reinhardtites levis Prins & Sissingh in Sissingh 1977
Retecapsa sp.
Stradnerlithus sp.
Tortolithus sp.
Uniplanarius gothicus (Deflandre 1959) Hattner & Wise 1980
Uniplanarius sissinghii Perch-Nielsen 1986
Uniplanarius sp.
Quadrum gartneri Prins & Perch-Nielsen in Manivit et al. 1977
Quadrum svabenickae Burnett 1997
Quadrum sp.
Watznaueria barnesiae (Black in Black & Barnes 1959) Perch-
Nielsen 1968
Watznaueria biporta Bukry 1969
Watznaueria britannica (Stradner 1963) Reinhardt 1964
Watznaueria communis Reinhardt 1964
Watznaueria fossacincta (Black 1971) Bown in Bown & Cooper 1989
Watznaueria ovata Bukry 1969
Watznaueria manivitiae Bukry 1973
Watznaueria sp.
vi
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample no. / Schaubing
Abundance
Pr
eservation
Acanthoica
sp.
Braarudosphaera bigelowii
Calcidiscus leptoporus
Coccolithus pelagicus
Coccolithus
sp.
Coronosphaera mediterranea
Cyclicargolithus floridanus
Discoaster
sp.
Helicosphaera ampliaperta
(<10)
Helicosphaera ampliaperta
(>10)
Helicosphaera carteri
Helicosphaera mediterranea
Helicosphaera scissura
Helicosphaera vedderi
Helicosphaera
sp.
Pontosphaera multipora
Reticulofenestra ampliumbilicus
Reticulofenestra gelida
Reticulofenestra haqii
Reticulofenestra minuta
Reticulofenestra pseudoumbilicus
(5–7)
Reticulofenestra pseudoumbilicus
(>7)
Sphenolithus moriformis
Sphenolithus
sp.
Syracosphaera
cf.
pulchra
Umbilicosphaera rotula
Umbilicosphaera jafari
SCHB/37
B
SCHB/52
B
SCHB/65,4
B
SCHB/72
B
SCHB/74
B
SCHB/80
R
P
1
12
1
1
1
1
2
1
SCHB/90
F
MP
38
4
1
3
2
8
4
4
1
1
SCHB/100
F
MP
2
1
64
1
4
1
1
2
2
3
3
1
2
1
1
SCHB/116,2
R
MP
2
19
1
1
1
2
14
8
6
2
SCHB/120,7
FC
M
2
2
150
1
1
2
7
1
1
2
4
1
3
10
3
12
14
16
4
2
1
1
SCHB/124,8
FC
M
1
151
1
3
2
1
1
1
9
1
7
3
18
18
26
2
2
1
1
SCHB/130,6
FC MG
1
153
1
1
8
1
8
1
1
1
7
2
4
16
23
21
1
3
Calcareous nannofossils: Counts of the most important specimens in the well of Schaubing (48°15’28” N, 15°37’02” E).
Appendix C
vii
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Sample no. / Str
eithofen 1
Abundance
Pr
eservation
Coccolithus pelagicus
Cyclicargolithus floridanus
Helicosphaera ampliaperta
(<10)
Reticulofenestra haqii
Reticulofenestra minuta
Reticulofenestra pseudoumbilicus
(5–7)
Sphenolithus moriformis
Thoracosphaera
sp.
Mesozoic — r
eworked
Paleogene — r
eworked
STR-1/53,8
B
STR-1/151,5
VR
STR-1/249,3
B
STR-1/301,8
B
STR-1/351,2
B
STR-1/405
B
STR-1/451,9
B
STR-1/500,5
B
STR-1/554,8
B
STR-1/602,7
B
STR-1/654,8
VR
STR-1/754,5
B
STR-1/802
B
STR-1/853,8
VR
P
2
2
0
STR-1/854,9
B
STR-1/892,8
VR
P
3
2
1
1
5
1
STR-1/931
VR
M
2
1
1
1
1
STR-1/964,8
VR
M
1
2
1
STR-1/990,5
B
STR-1/1022,6
R
M
10
5
3
2
8
2
STR-1/1051,8
B
STR-1/1084,8
R
M
8
3
1
1
1
Calcareous nannofossils: Counts of the most important specimens in the well of Streithofen 1 (48°16’30” N, 15°57’12” E).
viii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
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, 2018, 69, 4, 315–334
Sample no. /
Altenmarkt
T1
Abundance
Pr
eservation
Acanthoica
sp.
Braarudosphaera bigelowii
Calcidiscus leptoporus
Calcidiscus pataecus
Calcidiscus
cf.
tr
opicus
Coccolithus miopelagicus
Coccolithus pelagicus
Coccolithus
sp.
Coronosphaera mediterranea
Cyclicargolithus floridanus
Discoaster
cf.
druggii
Discoaster
sp.
Hayaster perplexus
Helicosphaera ampliaperta
(<10)
Helicosphaera ampliaperta
(>10)
Helicosphaera mediterranea
Helicosphaera scissura
Helicosphaera vedderi
Helicosphaera
sp.
Reticulofenestra ampliumbilicus
Reticulofenestra gelida
Reticulofenestra haqii
Reticulofenestra minuta
Reticulofenestra pseudoumbilicus
(5-7)
Reticulofenestra pseudoumbilicus
(>7)
Sphenolithus moriformis
Sphenolithus multispinatus
Sphenolithus
sp.
Syracosphaera
cf
. pulchra
Syracospahera?
cf.
oneillii
Thoracosphaera
sp.
Umbilicosphaera jafari
Umbilicosphaera rotula
ALT-1/504,5
VR
ALT-1/509,5
FR
PM
2
1
44
1
1
2
1
1
3
3
1
2
1
2
4
ALT-1/560,0
C
M
22
190
13
2
1
1
1
1
67
ALT-1/580,0
R
M
3
40
2
2
2
1
1
1
4
8
2
1
1
ALT-1/603,0
VR
P
1
ALT-1/603,0(2)
VR
ALT-1/603,5
VR
PM
3
1
1
1
ALT-1/620,0
R
MP
1
8
1
2
1
1
ALT-1/640,0
R
M
7
1
37
5
1
1
1
5
2
1
1
2
ALT-1/670,0
VR
MP
1
6
1
1
3
ALT-1/690,0
VR
M
10
ALT-1/740,0
VR
M
1
1
1
25
2
1
1
1
2
1
1
1
1
ALT-1/760,0
VR
M
x
ALT-1/780,0
VR
M
x
1
ALT-1/801,4
B
ALT-1/830,0
B
x
ALT-1/870,0
R
MP
10
1
31
6
1
2
3
4
3
3
1
ALT-1/902,7
B
ALT-1/904,5 (1)
B
ALT-1/904,5 (2)
B
ALT-1/970,0
B
ALT-1/999,6
B
ALT-1/1030,0
B
ALT-1/1080,0
R
MP
3
1
45
2
1
1
1
2
6
9
4
3
ALT-1/1100,0
B
ALT-1/1140,0
R
MP
5
18
6
1
1
2
2
2
1
8
2
2
ALT-1/1203,5
VR
MP
4
1
1
1
ALT-1/1205,0 (1)
R
MP
2
5
3
1
Calcareous nannofossils: Counts of the most important specimens in the well of Altenmarkt T1 (48°34’59” N, 16°14’03” E).
ix
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
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, 2018, 69, 4, 315–334
Calcareous nannofossils: Counts of the most important specimens in the well of Laa 1 (48°42’28” N, 16°25’48” E).
Sample no. / Laa 1
Abundance
Pr
eservation
Braarudosphaera bigelowii
Calcidiscus leptoporus
Calcidiscus pataecus
Coccolithus pelagicus
Coronocyclus
cf.
nitescens
Coronosphaera mediterranea
Cyclicargolithus floridanus
Helicosphaera ampliaperta
(<10)
Helicosphaera ampliaperta
(>10)
Helicosphaera carteri
Helicosphaera scissura
Helicosphaera vedderi
Helicosphaera
sp.
Pontosphaera multipora
Reticulofenestra ampliumblicus
Reticulofenestra haqii
Reticulofenestra minuta
Reticulofenestra pseudoumbilicus
(5–7)
Reticulofenestra pseudoumbilicus
(>7)
Sphenolithus moriformis
Sphenolithus
sp.
Syracosphaera
cf.
pulchra
Syracosphaera?
cf.
oneillii
Thoracosphaera
sp.
Triquetrorhabdulus
sp.
LAA-1/900,0
VR
M
6
2
3
4
17
9
1
LAA-1/980,0
VR
MP
11
1
2
1
LAA-1/1020,0
RVR
M
LAA-1/1060,0
VR
M
56
1
2
1
2
1
5
1
1
1
4
LAA-1/1080,0
RVR
M
6
1
1
LAA-1/1140,0
RVR
M
7
1
1
LAA-1/1180,0
VR
M
26
1
64
42
5
3
1
1
116 14
2
LAA-1/1260,0
FR
M
8
54
5
1
8
2
1
1
2
1
1
2
2
2
LAA-1/1320,0
VR
M
16
1
76
2
3
1
1
1
LAA-1/1340,0
VR
M
4
1
2
4
LAA-1/1360,0
B
LAA-1/1390,0
B
LAA-1/1450,0
B
LAA-1/1480,0
B
LAA-1/1630,0
VR
M
4
LAA-1/1633,2
B
LAA-1/1633,7(1)
B
LAA-1/1633,7(2)
B
LAA-1/1636,5
B
LAA-1/1660,0
B
LAA-1/1700,0
B
LAA-1/1750,0
B
LAA-1/1795,4
B
LAA-1/1796,5(1)
B
LAA-1/1796,5(2)
B
LAA-1/1797,0
B
LAA-1/1798,9
B
LAA-1/1810,0
B
LAA-1/1840,0
B
LAA-1/1870,0
VR
M
4
1
2
1
LAA-1/1920,0
R
M
46
1
1
3
1
1
2
4
21
1
9
1
2
LAA-1/1940,0
VR
MP
1
3
1
4
2
1
LAA-1/2000,0
F
M
52
2
1
1
2
2
5
4
3
18
2
x
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample no. /
W
ildendürnbach K4
Abundance
Pr
eservation
Acanthoica
sp.
Braarudosphaera bigelowii
Calcidiscus leptoporus
Calciosolenia fossilis
Coccolithus miopelagicus
Coccolithus pelagicus
Coccolithus
sp.
Coronocyclus baileyi
Coronocyclus
cf.
nitescens
Coronosphaera mediterranea
Cyclicargolithus floridanus
Discoaster deflandrei
Discoaster
sp.
Helicosphaera ampliaperta
(<10)
Helicosphaera ampliaperta
(>10)
Helicosphaera carteri
Helicosphaera intermedia
Helicosphaera mediterranea
Helicosphaera scissura
Helicosphaera vedderi
Lithostromation
sp.
Pontosphaera multipora
Reticulofenestra ampliumbilicus
Reticulofenestra gelida
Reticulofenestra haqii
Reticulofenestra minuta
Reticulofenestra pseudoumbilicus
(5–7)
Sphenolithus conicus
Sphenolithus heteromorphus
Sphenolithus moriformis
Sphenolithus
sp.
Syracospahera
cf.
pulchra
Syracosphaera?
cf.
oneillii
Thoracosphaera
sp.
Triquetrorhabdulus
sp.
Umbilicosphaera jafari
WDK-4/752
FC
PM
6
1
97
1
1 11
1
1 23 37 2
3
1
1
1
4
5
9
5
1
5
3
3
1
WDK-4/854,5
F
M
1
1
1
1
92
1
3
1
2
1
1
30
10
7
1
3
13 17 3
1
5
1
1
1
1
WDK-4/905(2)
F
MP
1
1
53
1
3
2
1
1
4
8
2
1
4
1
1
WDK-4/953,5
R/VR
P
2
29
1
3
1
3
7
4
5
2
1
2
WDK-4/954,8
B
WDK-4/996,5(2)
VR
P
4
3
1
WDK-4/1051
B
WDK-4/1051,9
F
M
1 13
147
4
3
8
1
12
1
1
5 12 6
3
1
1
3
WDK-4/1054,2
B
WDK-4/1054,8
R
MP
2
29
1
2
2
2
4
2
1
5
5
3
2
2
1
WDK-4/1095,4(2)
B
WDK-4/1154,5(2)
B
WDK-4/1201,5(1,2)
B
WDK-4/1202,35
B
WDK-4/1254,3 (2)
FC
MP
1
7
165 2
2
2
1
1
1
1
5
3
1 14 7
3
1
2
3
WDK-4/1301,1
B
WDK-4/1303
B
WDK-4/1351,8
B
WDK-4/1353
B
WDK-4/1402,6
B
WDK-4/1403,6
B
WDK-4/1453,25
B
WDK-4/1504
B
Calcareous nannofossils: Counts of the most important specimens in the well of Wildendürnbach K4 (48°44’58” N, 16°30’51” E).
xi
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Well
Sample
Well Depth (m)
Counted Specimens
Wildendürnbach K4
2014-WDK4 752
752.0
311
Wildendürnbach K4
2014-WDK4 854,5
854.5
301
Wildendürnbach K4
2014-WDK4 905
905.0
105
Wildendürnbach K4
2014-WDK4 953,5
953.5
35
Wildendürnbach K4
2014-WDK4 954,8
954.8
0
Wildendürnbach K4
2014-WDK4 996,5
996.5
18
Wildendürnbach K4
2014-WDK4 1051,7
1051.7
0
Wildendürnbach K4
2014-WDK4 1051,9T
1051.9
131
Wildendürnbach K4
2014-WDK4 1054,2
1054.2
0
Wildendürnbach K4
2014-WDK4 1054,8
1054.8
51
Wildendürnbach K4
2014-WDK4 1095,4
1095.4
0
Wildendürnbach K4
2014-WDK4 1154,5
1154.5
0
Wildendürnbach K4
2014-WDK4 1201,5
1201.5
0
Wildendürnbach K4
2014-WDK4 1202,35
1202.3
0
Wildendürnbach K4
2014-WDK4 1254,3
1254.3
307
Wildendürnbach K4
2014-WDK4 1301,1
1301.1
0
Wildendürnbach K4
2014-WDK4 1303
1303.0
0
Wildendürnbach K4
2014-WDK4 1351,8
1351.8
0
Wildendürnbach K4
2014-WDK4 1353
1353.0
0
Wildendürnbach K4
2014-WDK4 1402,6
1402.6
0
Wildendürnbach K4
2014-WDK4 1403,6
1403.6
0
Wildendürnbach K4
2014-WDK4 1453,35
1453.3
0
Wildendürnbach K4
2014-WDK4 1504,5T
1504.5
0
Well
Sample
Well Depth (m)
Counted Specimens
Schaubing
2014-Schb 65,4
65.4
10
Schaubing
2014-Schb 72
72.0
26
Schaubing
2014-Schb 80
80.0
209
Schaubing
2014-Schb 90
90.0
200
Schaubing
2014-Schb 100
100.0
102
Schaubing
2014-Schb 116,2
116.2
400
Schaubing
2014-Schb 120,7
120.7
226
Schaubing
2014-Schb 124,8
124.8
203
Schaubing
2014-Schb 130,6
130.6
179
Appendix D
Appendix E
Calcareous Nannofossils: Total counts per sample
Dinoflagellate cysts: Total counts per sample
xii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
01/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Low. A. Ernstbrunn 16.30749424
48.51999682
Iron bearing Sands
and Clays
Claystone
02/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Low. A. Ernstbrunn 16.28944408
48.47472236
Iron bearing Sands
and Clays
Clay
03/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Up. A. Gurten
13.34361233
48.24916164
Wildendürnbach
Formation
Fine grained Sand
04/17.04
0
Sample
Concretion
-
-
-
-
-
-
-
-
-
-
- Up. A. Gurten
13.34361233
48.24916164
Wildendürnbach
Formation
Fine grained Sand
05/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Up. A. Roßbach
13.23944964
48.18721279
Wildendürnbach
Formation
Sand
06/17.04
0
Sample
Fossilien (Oncophora)
-
-
-
-
-
-
-
-
-
-
- Up. A. Roßbach
13.23944964
48.18721279
Wildendürnbach
Formation
Sand
07/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Up. A. Roßbach
13.23944964
48.18721279
Wildendürnbach
Formation
Siltstone
08/17.04
0
Sample
-
-
-
-
-
-
-
-
-
-
- Up. A. Roßbach
13.23944964
48.18721279
Wildendürnbach
Formation
Sand
2014-05 I
0
Sample
Konkretionen aus Basis
-
-
-
-
-
-
-
-
-
- 4 Low. A. St. Pölten
15.62278165
48.22194085
Traisen Formation Silt, Sand, Fine grained
Gravel
2014-06 I
0
Sample
Sand
1 - 1 -
-
-
-
- 1 -
- Low. A. St. Pölten
15.62278165
48.22194085
Traisen Formation Silt, Sand, Fine grained
Gravel
2014-07 I
0
Sample
direkt über laminiertem: schräg-Geschichtete Schichten, Grobsand mit
Feinkies
1 - 1 -
-
-
-
- 1 -
- Low. A. St. Pölten
15.62278165
48.22194085
Traisen Formation Silt, Sand, Fine grained
Gravel
2014-11 I
0
Sample
1 - 1 -
-
-
-
- 1 -
- Low. A. Dietersdorf 15.96000442
48.25861174
Dietersdorf
Formation
Conglomerate
2014-12 I
0
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A. Pixendorf
15.96944347
48.28110576
Traisen Formation Fine grained Gravel,
Sand
2014-WDK4
1562,4
1562.4
Sample
1 -
-
-
-
- 1 - 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Bioturbated
Sandstone
Very fine grained Sand,
Siltstone, unknown
2014-WDK4
1563
1563
Sample
1 - 1 1 -
- 1 - 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Bioturbated
Sandstone
Very fine grained Sand,
Glaukonitsandstein
2014-WDK4
1531,7
1531.7
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Siltstone
2014-WDK4
1532,5
1532.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Siltstone
2014-WDK4
1504,7
1504.7
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Siltstone
List of samples and adjacent data.
Appendix F
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xiii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-WDK4
1452,4
1452.4
Sample
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand, Very
fine grained Sand,
Arkose
2014-WDK4
1453
1453
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand, Very
fine grained Sand
2014-WDK4
1453,35
1453.35
Sample
fine laminated carbonate poor siltstone
1 - 1 - 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Fine grained
Sand, Very fine grained
Sand
2014-WDK4
1453,5
1453.5
Sample
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand, Very
fine grained Sand,
Arkose
2014-WDK4
1454,85
1454.85
Sample
light grey massive to deformed Sand, dark grey carbonate free
1 -
-
-
- 1 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Very fine grained Sand,
Fine grained Sand,
Arkose
2014-WDK4
1455
1455
Sample
carbonate free, light grey
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand, Very
fine grained Sand
2014-WDK4
1401,65
1401.65
Sample
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Very fine grained Sand,
Arkose
2014-WDK4
1401,75
1401.75
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite
2014-WDK4
1402
1402
Sample
pps, massive
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Very fine grained Sand,
Arkose
2014-WDK4
1402,5
1402.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite
2014-WDK4
1403
1403
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite
2014-WDK4
1403,6
1403.6
Sample
1 1 1 - 1 -
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Very fine grained
Sand
2014-WDK4
1404,2
1404
Sample
laminated dark Siltstone
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand
2014-WDK4
1404,7
1404.7
Sample
dark fine banked
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite
2014-WDK4
1351,3
1351.3
Sample
massive Sandstone, coarsening upwards
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Medium Grained Sand,
Lithic Arkose
2014-WDK4
1351,5
1351.5
Sample
massive Sandstone
1 -
-
-
- 1 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Coarse Grained Sand,
Lithic Arkose
2014-WDK4
1351,8
1351.8
Sample
marly
1 -
-
- 1 -
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Silt, Pelite
2014-WDK4
1353
1353
Sample
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Silt
2014-WDK4
1354,2
1354.2
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Pelite, Silt
2014-WDK4
1355
1355
Sample
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Wildendürnbach
Formation
Fine grained Sand, Very
fine grained Sand, Lithic
Arkose
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xiv
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-WDK4
1301,1
1301.1
Sample
1 - 1 1 1 -
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1303
1303
Sample
rich in plants
1 -
-
- 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1304
1304
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Pelite
2014-WDK4
1304,5
1304.5
Sample
Fe-bearing clasts, fining upwards
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand,
Medium Grained Sand,
Arkose
2014-WDK4
1305
1305
Sample
carbonate poor
1 -
-
-
-
-
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite, Very fine grained
Sand
2014-WDK4
1300
1300
Sample
Top of Turpedite
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1300,5
1300.5
Sample
Sandlinsen, großer Schliff
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Sandstone, Feldspathic
Wacke
2014-WDK4
1254,3
1254.3
Sample
ripples, light grey, poor in mica
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1254,4
1254.4
Sample
ripples, light grey, poor in mica, top of turpedite
1 -
-
-
- 4 1 - 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1254,5
1254.5
Sample
ripples, light grey, poor in mica
1 -
- 1 -
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Silt, Wacke
2014-WDK4
1254,9
1254.9
Sample
light grey, poor in mica
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1256,3
1256.3
Sample
micaceous, Top of small turpedite
1 -
-
-
-
- 1 - 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite, Very fine grained
Sand
2014-WDK4
1256,8
1256.8
Sample
poorly sorted
1 - 1 -
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Medium Grained Sand,
Coarse Grained Sand,
Feldspathic Wacke
2014-WDK4
1201,4
1201.4
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand
2014-WDK4
1201,5
1201.5
Sample
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xv
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-WDK4
1201,6
1201.6
Sample
ripples
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Arkose
2014-WDK4
1201,95
1201.95
Sample
bouma Sequence, fining upwards, ripples
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand, Very
fine grained Sand,
Arkose
2014-WDK4
1202,35
1202.35
Sample
1 -
-
- 1 -
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1202,5
1202.5
Sample
1 1 -
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1202,7
1202.7
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand
2014-WDK4
1204,5
1204.5
Sample
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand,
Arkose
2014-WDK4
1151,5
1151.5
Sample
1 -
-
-
- 4 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Medium Grained Sand,
Lithic Arkose
2014-WDK4
1152,2
1152.2
Sample
fining upwards
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Medium Grained Sand,
Fine grained Sand,
Lithic Arkose
2014-WDK4
1152,5
1152.5
Sample
coarsening
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Fine grained Sand
2014-WDK4
1153
1153
Sample
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand
2014-WDK4
1154
1154
Sample
fining upwards
1 1 1 -
- 1 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Medium Grained Sand,
Fine grained Sand,
Arkose
2014-WDK4
1154,2
1154.2
Sample
Pelite-Sand Intrelayering
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite, Sand
2014-WDK4
1154,5
1154.5
Sample
Pelite-VF-Sand interlayering
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Pelite
2014-WDK4
1150,5
1150.5
Sample
sandy and marly banks
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Medium Grained Sand
2014-WDK4
1095,4
1095.4
Sample
dark grey brownish grey Siltstone, changing SO3 content
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xvi
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-WDK4
1095,8
1095.8
Sample
dark grey brownish grey Siltstone, changing SO3 content
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite, Feldspathic
Wacke
2014-WDK4
1051h
1051
Sample
changing marl content
1 - 1 1 1 -
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1051,7
1051.7
Sample
consolidated
1 -
-
- 1 -
-
- 1 1 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand,
Feldspathic Wacke
2014-WDK4
1053,3
1053.3
Sample
strongly consolidated FS
1 1 -
-
-
- 1 - 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Fine grained Sand
2014-WDK4
1053,6
1053.6
Sample
marly Siltstone
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1054
1054
Sample
marly Siltstone, Fe-rich
1 -
-
-
-
- 1 - 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
1054,5
1054.5
Sample
debris flow; Clay Clasts, strongly consolidated, clay minerals
1 1 -
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Feldspathic Wacke, Fine
grained Sand, Silt
2014-WDK4
1054,8
1054.8
Sample
1 -
-
- 1 -
-
- 1 7 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Transition Facies
Ottnangian/
Karpatian
Pelite
2014-WDK4
996,5
996.5
Sample
light grey Siltstone with changing marl-content
1 - 1 - 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-WDK4
953,5
953.5
Sample
1 1 -
- 1 -
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-WDK4
953,7
953.7
Sample
consolidated
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Fine grained Sand
2014-WDK4
953,9
953.9
Sample
consolidated
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Fine grained Sand,
Feldspathic Wacke
2014-WDK4
954,7
954.7
Sample
clay clasts
1 -
-
-
- 4 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Medium Grained Sand,
Fine grained Sand,
Wacke
2014-WDK4
954,8
954.8
Sample
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-WDK4
903,7
903.7
Sample
ripples, pps, fining upwards
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Very fine grained Sand,
Fine grained Sand,
Arkose
2014-WDK4
904,5
904.5
Sample
coarsening, poorly consolidated
1 1 -
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Very fine grained Sand,
Arkose
2014-WDK4
904,7
904.7
Sample
poorly consolidated sheeted FS + plants, Xrd indicates Fe-rich composition 1 - 1 -
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Fine grained Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xvii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-WDK4
905
905
Sample
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-WDK4
854
854
Sample
Drill Gouge
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Drill Gouge
2014-WDK4
854,5
854.5
Sample
marly Siltstone
1 - 1 1 1 -
-
- 1 1 - Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-WDK4
802,2
802.2
Sample
poorly consolidated
1 1 1 -
- 1 -
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Medium Grained Sand,
Feldspathic Wacke
2014-WDK4
803,2
803.2
Sample
poorly consolidated
1 -
-
-
-
-
-
- 1 -
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Coarse Grained Sand
2014-WDK4
805
805
Sample
poorly consolidated
1 -
-
-
-
-
-
- 1 - 1 Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Coarse Grained Sand,
Arkose
2014-WDK4
752
752
Sample
slightly marly silts, CO3 rich and mica-poor; poorly consolidated
1 -
-
- 1 -
-
-
-
-
- Low. A.
Wildendürnbach
16.51372494
48.75002006
Wildendürnbach
K4
Laa Formation
Pelite
2014-Schb
130,6
130.6
Sample
kalkhaltiger grauer Silt mit Fischschuppen nahe Basis
1 - 1 1 1 -
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb
124,8
124.8
Sample
hellgrauer mergeliger Silt ==> für Schwerminerale
1 5 1 1 1 -
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb
120,7
120.7
Sample
grauer Silt-Feinsand, strukturlos; immer wieder Siltlagen im Pelit
1 5 1 1 1 - 1 - 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt, Fine grained Sand
2014-Schb
116,2
116.2
Sample
Grobsand + Pelit, mergelig, massig grau; Schneiden!!
GrobsandLage gefolgt von siltig tonigen hell/dunkelgrau mm laminierten
Schichten, 10cm höher dann eine 5cm dicke feinsandige Lage mit einem
leichten fining upward. ==> flachmarine ruhige sedimentation o
1 1 1 1 1 -
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Coarse Grained Sand,
Silt
2014-Schb 100
100
Sample
grauer siltiger Mergel; Schneiden!!
Mehrere cm dicke dunkle feinkörnige (Ton-Silt) Lage unterbrochen von
mm-cm dicken gröberen hellgrauen Lagen. Die hellgrauen Lagen sind
Grobsilt-SF-Sand; eine mehrere mm dicke Lage zeigt komplexe
linsenartige Strukturen
1 5 1 1 1 -
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb 90
90
Sample
grauer siltiger Mergel; Fischschuppen
aufgeschnitten: mm-cm dicker eben laminierter hell/dunkerlgrauer Fein-
Grobsilt, gröbere u. feinere Bereiche wechseln
1 5 1 1 1 -
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb 80
80
Sample
grauer siltiger Mergel; Fischschuppen
Aufgeschnitten: mm dicker hell/dunkelgrauer eben laminierter siltiger
Mergel
1 - 1 1 1 -
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb 74
74
Sample
fein laminierte hellgraue Silte, teils bräunlich-dunkel verfärbt, kalkfrei +
Gipsblüten
1 - 1 1 1 -
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt
2014-Schb 72
72
Sample
Silt-Feinsande, kalkfrei, hellgrau, keine bation?Gipsblüten, angeschnitten
sind Strukturen erkennbar, Biotur
1 1 1 1 1 -
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Silt, Fine grained Sand
2014-Schb 65,4 65.4
Sample
teils dunkle Lagen reich an org. Material, Gipsblüten, kalkfrei
1 - 1 1 1 - 1 - 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Silt
2014-Schb 52
52
Sample
kalkfreie tonige Silte, hellgrau, keine Gipsblüten
1 - 1 1 1 -
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Silt
2014-Schb 37
37
Sample
FS, kalkarm, Pflanzenreste, gelblich rötlich
1 5 1 1 1 -
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Fine grained Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xviii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Schb 24
24
Sample
verfestigter gradierter MS-FS kalkreich ==> Schneiden/Dünnschliff,
angeschnitten ein strukrurloser stark verfestigter Mittelsand
1 1 1 -
-
-
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Medium Grained Sand
2014-Schb 16,3 16.3
Sample
MS, rötlich, verfestigt, kalkfrei;
Augeschnitten: strukturloser stark verfestigter Mittelsand
1 5 1 -
-
-
-
- 1 - 2 Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Medium Grained Sand
2014-Laa 1799
1799
Sample
fine sand, convolute bedding,
1 4 1 -
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Fine grained Sand
2014-Laa
1798,4
1798.4
Sample
graublaue Hintergrundsedimentation
1 - 1 4 1 - 1 - 1 7 - Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay
2014-Laa 1797
1797
Sample
FS-Ms + Clay clasts
1 6 -
- 1 -
- 1 1 - 6 Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Sand
2014-Laa
1796,5
1796.5
Sample
Mud + Sand. Viel Straukturen
1 -
-
- 1 -
- 1 1 - 6 Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud, Sand
2014-Laa
1795,8
1795.8
Sample
Mud und helle Linsen
1 -
- 4 1 -
-
- 1 7 - Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-Laa
1795,3
1795.3
Sample
silitiger Mud, finning upward
1 -
-
-
-
-
- 1 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-Laa 1638
1638
Sample
MS
- 4 -
-
-
-
-
-
-
- 5 Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Medium Grained Sand
2014-Laa
1636,5
1636.5
Sample
MS-Mud-MS, Entwässerungsstrukturen
1 -
-
- 1 -
- 1 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1635,5
1625.5
Sample
MS
- 1 -
-
-
-
-
-
-
- 5 Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Medium Grained Sand
2014-Laa 1636
1636
Sample
Mud-MS
-
-
-
-
-
-
- 1 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1633,7
1633.7
Sample
MS-Mud-MS-Mud
1 -
-
- 1 -
- 1 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1633,2
1633.2
Sample
Mud
1 - 1 4 1 -
-
- 1 7 - Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-AltT1
1205
1205
Sample
Jura Kalk ==> Basis Eggenburg, Ms, Gradient: Schwarze Minerale werden
nach oben hin weniger
1 6 -
- 1 -
- 1 1 7 6 Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Carbonate Arenite
Serie
unknown
2014-AltT1
1203,3
1203.3
Sample
Bioturbated Sand
1 -
- 4 1 -
-
-
- 1 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Bioturbated
Sandstone
Sand
2014-AltT1
1201,5
1201.5
Sample
Bioturbated Sand
1 4 -
-
-
- 1 - 1 - 5 Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Bioturbated
Sandstone
Sand
2014-AltT1
1001,5
1001.5
Sample
Sand, MS-FS, Entwässerungsstrukturen
1 6 -
-
-
-
- 1 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Sand
2014-AltT1
999,8
999.8
Sample
MS-Mud und Feinkies
-
-
-
-
-
-
- 1 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
unknown
2014-AltT1
904,5
904.5
Sample
MS-Mud-MS
-
-
-
- 1 -
- 1 1 - 6 Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
unknown
2014-AltT1
903,5
903.5
Sample
MS
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Medium Grained Sand
2014-AltT1
902,7
902.7
Sample
Mud
-
-
- 4 1 -
-
-
-
-
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mud
2014-AltT1
901,3
901.3
Sample
Mud (ohne Sandlage)
1 - 1 -
-
-
-
- 1 1 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mud
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xix
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-AltT1
900,5
900.5
Sample
CS-MS-Cs
1 4 -
-
-
-
-
- 1 - 5 Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Coarse Grained Sand
2014-AltT1
803,5
803.5
Sample
Sand
1 1 1 -
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Sand
2014-AltT1
802,8
802.8
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Sand
2014-AltT1
801,4
801.4
Sample
Mud
1 -
-
- 1 -
- 1 1 7 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Mud
2014-AltT1
603,5
603.5
Sample
Mud
1 -
- 4 1 -
-
-
- 1 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mud
2014-AltT1 603 603
Sample
Mud, Sand, komplexe Strukturen
-
-
-
- 1 -
- 1 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
unknown
2014-AltT1 602 602
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Sand
2014-AltT1
504,5
504.5
Sample
Marl
1 -
-
- 1 -
- 1 1 1 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Marl
2014-Por2 1358 1358
Sample
Glaukonitsandstein
-
-
-
-
-
-
- 1 1 - 6 Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Glaukonitsandstein
2014-Por2
1357,5
1357.5
Sample
Glaukonitsandstein
1 4 -
-
-
-
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Glaukonitsandstein
2014-Por2 1294 1294
Sample
aufgearbeiteter Glaukonitsandstein
1 4 1 -
-
-
- 1 1 - 5 Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Glaukonitsandstein
2014-Por2
1255,5
1255.5
Sample
Bioturbierte Fischfazies?
1 4 - 4 1 - 1 1 1 7 5 Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Sand
2014-Por2
1102,5
1102.5
Sample
brauner Mud
1 -
- 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mud
2014-Por2 1005 1005
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Sand
2014-Por2
1004,5
1004.5
Sample
hellbrauner (1; XRF 109) und dunkelbrauner (2; XRF 110) Mud; XRD: ID
1213-1219 entspricht 2.; ID 1220-1226 entspricht 1.; CO3: ID 123
entspricht 1.; ID 124 entspricht 2.;
1 -
- 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mud
2014-Por2
1004,8
1004.8
Sample
Sand und Pflanzenhäcksel
-
-
-
-
-
-
- 1 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Sand
2014-Por2 857
857
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Sand
2014-Por2 856,5 856.5
Sample
brauner Mud
1 -
- 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mud
2014-Por2 704
704
Sample
hellbrauner Mud
1 -
- 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mud
2014-Por2 554,4 554.4
Sample
Sand-Mud, fining upward
-
-
-
- 1 -
- 1 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-Por2 552,5 552.5
Sample
Sand + Clay Clasts
1 1 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xx
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Por2 552
552
Sample
dunkelbrauner Mud
1 -
- 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mud
2014-Por2 437
437
Sample
Mud
1 - 1 4 1 -
-
- 1 7 - Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-Por2 437,5 437.5
Sample
VF Sand
1 4 -
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mud, Very fine grained
Sand
2014-Mail2
1455
1455
Sample
Jurakalk
-
-
-
-
-
-
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Carbonate Reef
Marble
2014-Mail2
1381
1381
Sample
Sand, hellgrau, gelb +Pflanzenreste; eher eckige schlecht sortierte Sande,
(lokal?);
1 6 -
-
-
-
- 1 1 - 6 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sand
2014-Mail2
1330,5
1330.5
Sample
Sand
1 4 -
-
-
-
-
- 1 - 5 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sand
2014-Mail2
1329,5
1329.5
Sample
zementierter Sand
1 1 -
-
-
-
-
- 1 - 5 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sandstone
2014-Mail2
1269
1269
Sample
Sand
1 1 1 -
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sand
2014-Mail2
1266
1266
Sample
zementierter Sand; zementierte Bereiche stark durchwühlt
-
-
-
-
-
-
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sandstone
2014-Mail2
1210
1210
Sample
Ton, Fischschuppen
1 - 1 4 1 - 1 - 1 1 - Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Clay
2014-Mail2
1115
1115
Sample
Grobsand
1 1 -
-
-
-
-
- 1 - 5 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Coarse Grained Sand
2014-Mail2
1114,5
1114.5
Sample
unverfestigter Sand + Muschelreste, vermutlich Luciniden-Reste, die
vollmarine Bedingungen andeuten
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Sand
2014-Mail2
1114
1114
Sample
zementierter Sand + Clay Clasts
-
-
-
- 1 -
- 1 1 - 6 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Sandstone
2014-Mail2 978 978
Sample
Sand-Ton Wechsellagerung; distales Delta?
-
-
-
- 1 -
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
unknown
2014-Mail2 977 977
Sample
Sand-Ton Wechsellagerung; distales Delta?
-
-
-
- 1 -
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
unknown
2014-Mail2 976 976
Sample
Sand-Ton Wechsellagerung; distales Delta?
-
-
-
- 1 -
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
unknown
2014-Mail2 975 975
Sample
Ton/Mud
1 -
- 4 1 -
-
- 1 1 - Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mud
2014-Mail2 875 875
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 753 753
Sample
FS, ripples, Top of Turpedit?
1 1 - 4 1 -
-
- 1 1 - Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Fine grained Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxi
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Mail2
752,5
750.5
Sample
Sand
1 1 -
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2
751,5
751.5
Sample
Mud-Sand
-
-
-
- 1 -
- 1 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
unknown
2014-Mail2 655 655
Sample
zementierter Konglomerat + Sand
-
-
-
-
-
-
- 1 1 - 6 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Conglomerate
2014-Mail2 653 653
Sample
Sand
1 6 -
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 651 651
Sample
Konglomerat unverfestigt (Flussschotter?);
- 7 -
-
-
-
-
-
-
-
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Conglomerate
2014-Mail2 554 554
Sample
Sand
1 6 -
-
-
-
-
- 1 - 6 Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-AltT1
999,6
999.6
Sample
gelblicher Mud
1 -
- 4 1 -
-
- 1 1 - Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mud
2014-Por2 1254 1254
Sample
Bioturbierte Fischfazies?
1 4 - 4 1 -
- 1 1 7 5 Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Sand
2015-01/01 I
0
Sample
Sandlage, Karbonat und Augensteine gemischt
1 6 -
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Quatenary Lake
Sediments
Coarse Grained Sand
2015-01/01 II
0
Sample
dirty sample of quatenary sand including augenstein formation
-
-
-
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Quatenary Lake
Sediments
Coarse Grained Sand
2015-01/01 III
0
Sample
Clay sample. Quatenary lake clays?
-
-
-
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Quatenary Lake
Sediments
Clay
2015-01/01 IV
0
Sample
Paleosol
-
-
-
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Paleosol
Clay
2015-01/01 V
0
Sample
Large sample for sieving
1 -
-
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Quatenary Lake
Sediments
Coarse Grained Sand
2015-01/02 I
0
Sample
quatenary lake sediments?
1 6 -
-
-
-
-
-
-
- Low.A. Mailberg
15.26308389
47.68774639
Quatenary Lake
Sediments
Coarse Grained Sand
2015-01/03 I
0
Sample
In situ Augensteine? Strongly weathered, deep soils,
1 6 -
-
-
-
-
-
-
-
- Low.A. Mailberg
15.26225971
47.68814417
Augenstein
Formation
Conglomerate
2015-01/01 VI
0
Sample
large components
-
-
-
-
-
-
-
-
-
- Zellersteritzen
15.26445371
47.68721238
Quatenary Lake
Sediments
Conglomerate
2015-Laa1 1020 1020
Sample
(cuttings)
Cuttings: hellgrau, cm groß, kugelig bis plattig, verklumpend
Lithologie: vorwiegend Ton
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton >
Silt
2015-Laa1 1040 1040
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm groß, plattig, teilweise verklumpend
Lithologie: Ton/Silt
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton >
Silt
2015-Laa1 1060 1060
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm groß, meist plattig
Lithologie: CO3 zemetierte Sande, Qz-Kiese, Silte, Tone
Verunreinigung: magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt/
Sand/Feinkies
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1070 1070
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm groß, vorwiegend plattig, leicht
verklumpend
Lithologie: vorwiegend Tone u. Silte, Sandstücke CO3 zementiert
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-Laa1 1080 1080
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm groß, meist plattig
Lithologie: Silte überwiegen
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-Laa1 1100 1100
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm gr0ß, vorwiegend plattig
Lithologie: alles dabei, Sande oft CO3 zementiert
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Laa1 1120 1120
Sample
(cuttings)
Cuttings: hellgrau, mm-1cm groß, vorwiegend plattig, einzelne
Mineralkörner, wenig Material
Lithologie: alles dabei, glimmerführend
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Laa1 1140 1140
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm groß, kugelig bis plattig, teilweise
verklumpend
Lithologie: Silte, VFSande u. Tone
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-Laa1 1160 1160
Sample
(cuttings)
Cuttings: hellgrau, mm.2cm groß, kugelig u. plattig
Lithologie: Fsande mit eingebetteten gröberen Komponenten
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt > Sand
2015-Laa1 1180 1180
Sample
(cuttings)
Cuttings: hellgrau 0,5cm-2cm groß, kugelig bis plattig, verklumpend
Lithologie: Tonreich, meist Siltüberzogen
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton >
Silt
2015-Laa1 1200 1200
Sample
(cuttings)
Cuttings: hellgrau, 0,5mm-3cm groß, blättrig bis kugelig
Lithologie: glimmerige Fsande u. Silte mit gröberen Komponenten
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt > Sand
2015-Laa1 1240 1240
Sample
(cuttings)
Cuttings:
Lithologie:
Verunreinigung:
Qualität 1-5:
-
-
-
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
unknown
2015-Laa1 1260 1260
Sample
(cuttings)
Cuttings: hellgrau, mm-cm groß, blättrig bis kugelig, leicht verklumpend,
wenig Material
Lithologie: glimmerführende Silte/Fsande mit gröberen Komponenten
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt > Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxiii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1290 1290
Sample
(cuttings)
Cuttings: hellgrau, 0,5-2cm groß, kugelig, verklumpend, wenig Material
Lithologie: glimmereiche Silte u. Feinsande, größere Körner teilweise in
FS/Silt-Matrix eingebettet
Verunreinigung: wenige Pflanzenreste
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt > Sand
2015-Laa1 1310 1310
Sample
(cuttings)
Cuttings: hellgrau, mm-cm, blättrig bis kugelig, stark verklumpend
Lithologie: glimmereiche Silte u. Sande
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt
2015-Laa1 1320 1320
Sample
(cuttings)
Cuttings: mittelgrau, cm groß, kugelig, selten blättrig
Lithologie: MS-FS, Silte, teilweise glimmerreich
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
unknown
2015-Laa1 1330 1330
Sample
(cuttings)
Cuttings: mittelgrau, mm-1,5cm, blättrig bis kugelig
Lithologie: glimmereicher Feinsand, Silt, auch Ton, wenige Qz-Körener
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt/
VFSand
2015-Laa1 1340 1340
Sample
(cuttings)
Cuttings: hellgrau, 0,5mm-2cm groß, kugelig, selten blättrig
Lithologie: glimmereiche Feinsande u. Silte
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample:
VFSand/Silt
2015-Laa1 1360 1360
Sample
(cuttings)
Cuttings: mittelgrau, mm-2cm, blättrig bis kugelig
Lithologie: Tone, glimmereiche Silte, wenige glimmereiche
Feinsandstücke
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt/
VFSand
2015-Laa1 1390 1390
Sample
(cuttings)
Cuttings: mittelgrau, mm-2cm, blättrig u. kugelig
Lithologie: Ton u. Silt, wenig Feinsand, Silt 50%
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt/
VFSand
2015-Laa1 1410 1410
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm, kugelig u. blättrig
Lithologie: viel Feinsand, wenig Silt u. Ton
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt > Ton
2015-Laa1 1430 1430
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm groß, kugelig oder Blättchen
Lithologie: Helle Feinsande u. Silte, kaum Tone
Verunreinigung: Bauschutt??
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt
2015-Laa1 1450 1450
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm große teils kugelige Stücke, wenig Material
Lithologie: Feinsande und Silte, kaum Tone
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxiv
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1460 1460
Sample
(cuttings)
Cuttings: sehr hellgrau, cm groß kugelig u. verklumpend
Lithologie: große Klumpen aus sehr feinem Sand bis Silt, sehr einheitliche
Zusammensetzung
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt
2015-Laa1 1480 1480
Sample
(cuttings)
Cuttings: sehr hellgrau, cm groß kugelig u. verklumpend
Lithologie: große Klumpen aus sehr feinem Sand bis Silt, sehr einheitliche
Zusammensetzung
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt
2015-Laa1 1510 1510
Sample
(cuttings)
Cuttings: hellbraun, mm-1cm große Stücke
Lithologie: ?
Verunreinigung: Gumme, extrem viele magnetische Stücke, Bauschutt,
Pflanzenreste
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
Feinkies/Sand
2015-Laa1 1530 1530
Sample
(cuttings)
Cuttings: hellgelb, bis 2cm große Stücke
Lithologie: Kies u. Sand? (schwer zu sagen aufgrund extremer
Verunreinigung)
Verunreinigung: extrem viele magnetische Stücke, Eisenspäne, Gumme,
Bauschutt, Asphalt?
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
Feinkies/Sand
2015-Laa1 1550 1550
Sample
(cuttings)
Cuttings: hellgelb, mm-cm groß, kugelig, grobkies
Lithologie:
Verunreinigung: extrem viele magnetische Stücke u. Eisenspäne, Gummi,
Schuttstücke
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample:
Feinkies/Sand
2015-Laa1 1570 1570
Sample
(cuttings)
Cuttings: hellgrau, gut gerundete mm-cm große Stücke,
Lithologie: Kies u. Dand
Verunreinigung: extrem viele magnetische Stücke u. Eisenspäne,
Pflanzenreste, Betonstücke, Asphalt??
Qualität 1-5: 6
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample:
Feinkies/Sand
2015-Laa1 1630 1630
Sample
(cuttings)
Cuttings: hellgrau, mm-cm große Blättchen, einzelne Klumpen, sehr
heterogen
Lithologie: viel Silt u. Feinsand, wenig Ton, mehrere Kohlestücke
Verunreinigung: sehr viele magnetische Stücke, Pflanzenreste
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample: Ton/Silt/
VFSand
2015-Laa1 1660 1660
Sample
(cuttings)
Größe der Cuttings: mm große elongierte Plättchen
Korngröße: Tone, wenig Silt
Lithologie: Tone, sehr wenige Stücke von Silt oder Sand
Verunreinigung: sehr viele Eisenspäne, einzelne Qz u. Fsp Körner
Qualität 1-5: 3 (sehr Homogen und gut aussehend auf ers
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay, Silt, Coal
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxv
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1700 1700
Sample
(cuttings)
Größe der Cuttings: mm-cm große Plättchen, cm große Kügelchen
Korngröße: Tone bis Feinsande
Lithologie: Ton-Chips, Silte und Feinsande, 30:30:30
Verunreinigung: viele Eisenspäne
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Coal, Clay, Silt, Sand
2015-Laa1 1720 1720
Sample
(cuttings)
Größe der Cuttings: mm große Plättchen und mm-cm große kugelige
Stücke
Korngröße: Tone bis Sande
Lithologie: Ton Chips, Silte und viel Feinsand >50%
Verunreinigung: kleine Eisenspäne
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay, Silt, Fine grained
Sand, Coal
2015-Laa1 1740 1740
Sample
(cuttings)
Größe der Cuttings: mm-cm große teilweise elongierte Plättchen, wenige
cm große Kugeln
Korngröße: Tone, Silte und Feinsande
Lithologie: Tone, Silte + Feinsande >50%
Verunreinigung: wenige kleine Eisenspäne
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2015-Laa1 1750 1750
Sample
(cuttings)
Größe der Cuttings: mm-cm große elongierte Plättchen und kugelige
Klumpen
Korngröße: sand bis ton
Lithologie: Ton-Chips und Feinsand-Stücke, Kohlestücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay, Fine grained Sand,
Coal, Silt
2015-Laa1 1770 1770
Sample
(cuttings)
Größe der Cuttings: mm große längliche Plättchen, wenige cm-große
kugelige Stücke
Korngröße: hauptsächlich Ton, wenig Silt oder Feinsand
Lithologie: Ton, wenig Feinsand <10%
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay, Silt, Very fine
grained Sand
2015-Laa1 1780 1780
Sample
(cuttings)
Größe der Cuttings: kleine cuttings (mm-Bereich), wenige cm große
Stücke
Korngröße: Silt-Ton, Feinsand 10-20 %
Lithologie: Glimmerführende Feinsande, Kohlen, Silte und Tone
Verunreinigung: Vorhanden aber gering, 1 Gummistück und wenige
Eisenstücke
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Clay, Very fine grained
Sand, Silt, Coal
2015-Laa1 1810 1810
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm große Blättchen
Lithologie: Tone, wenige Silte
Verunreinigung: einige magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Laa1 1820 1820
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm große Blättchen
Lithologie: Tone, wenige Silte, einzelne Klumpen
Verunreinigung:wenige Eisenstücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxvi
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1840 1840
Sample
(cuttings)
Cuttings: dunkelgrau, mm große Blättchen
Lithologie: Tone wenige Silte, einzelne Feinsandstücke, einzelne
Kiesstücke
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Laa1 1870 1870
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm große Blättchen, kogelige Klümpchen
Lithologie: Tone, wenige Silte
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Laa1 1920 1920
Sample
(cuttings)
Cuttings: dunkelgrau, hellere Stücke, mm-1cm große Blättchen
Lithologie: Tone, sehr wenige hellere-Siltstücke,
Verunreinigung: sehr wenige magnetische Stücke
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Laa1 1940 1940
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm große Blättchen
Lithologie: Tone, Silte, sehr wenige Sand-Stücke und einzelne Kies-Stücke
(Qz)
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Laa1 1950 1950
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1,5cm große Blättchen, wenige helle Stücke
Lithologie: Tone/Silte, Karbonate, CO3 zemntierte Sande
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Carbonate Arenite
Serie
Mixed Sample: Ton/Silt
> Carbonate/Sands
2015-Laa1 1970 1970
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm große Blättchen
Lithologie: Tone/Silte, karbonatische Stücke, CO3 zementierte Sandsteine
(sehr untergeordnet)
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Carbonate Arenite
Serie
Mixed Sample: Ton/Silt
> Carbonate
2015-Laa1 1990 1990
Sample
(cuttings)
Cuttings: dunkelgrau; wenige helle Stücke, mm-1cm große Blättchen
Lithologie: Tone, Silte, wenige Karbonate, einzelne kohlige Stücke
Verunreinigung: sehr wenige magnetische Stücke, 1 Eisenspan, 1
Pflanzenrest
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Carbonate Arenite
Serie
Mixed Sample: Ton/Silt
> Carbonate
2015-Laa1 2000 2000
Sample
(cuttings)
Cuttings: dunkelgrau, wenige helle Stücke, mm-1cm große Blättchen
Lithologie: Ton, Silt, wenige Kohle-Stücke, karbonatische Stücke
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Carbonate Arenite
Serie
Mixed Sample: Ton >
Silt
2015-Laa1 900
900
Sample
(cuttings)
Cuttings: hellgrau, mm-1cm groß, meist kleine Stücke oder große kugelige
Klumpen
Lithologie: Tonklasten mit Siltüberzug, CO3 zementierte Sandstücke,
feinkiesige Qz-Klasten
Verunreinigung: magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt
> Carbonate/Sands
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxvii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 940
940
Sample
(cuttings)
Cuttings: hellgrua, mm-1,5cm, meist plattig, verklumpend
Lithologie: Tonklasten mit Siltüberzug
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt
2015-Laa1 980
980
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm, plattig, selten kugelig, verklumpend
Lithologie: Tonklasten mit Siltüberzug
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Laa Formation
Mixed Sample: Ton/Silt
2015-AltT1
1030
1030
Sample
(cuttings)
Cuttings: hellgrau, <1cm, kantige Stücke
Lithologie: überwiegend FS u. Qz-Kies
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample: Sand >
Ton/Silt
2015-AltT1
1060
1060
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1,cm, meist plattig
Lithologie: Tone, wenig Silte, Qz-Körner u. CO3 zementierte Sande
Verunreinigung: viele magnetische Stücke, Pflanzenreste
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-AltT1
1080
1080
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm, plattig und kugelig verklumpend
Lithologie: stark verklumpte Aggregate aus Kies u. Ton, wenig Silt/Sand
Verunreinigung: wenig magnetische Stücke, Bauschutt?
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Robulus Schlier
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-AltT1
1100
1100
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm, plattig u. kugelig, verklumpend
Lithologie: Tonstücke überwiegen, selten Sand, einige einzelne
Mineralkörner verkittet in Klumpen
Verunreinigung: wenige magnetische Stücke, Bauschutt?
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Robulus Schlier
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-AltT1
1120
1120
Sample
(cuttings)
Cuttings: dunkelgrau, <1cm, plattig
Lithologie: Tonplattchen, untergeordnet, Feinkiesstücke (Qz) u. CO3
zementierte Sandstücke
Verunreinigung: magentische Stücke, Pflanzenreste
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Robulus Schlier
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-AltT1
1140
1140
Sample
(cuttings)
Cuttings: hellgrau, mm-1cm groß, meist kugelig, eckig
Lithologie: Hauptsächlich Feinsand
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Bioturbated
Sandstone
Mixed Sample: Sand >
Ton/Silt
2015-AltT1
1220
1220
Sample
(cuttings)
Cuttings: weiß, dunkle Stücke darin, < 0,5cm, plattig bis kugelig
Lithologie: Karbonate, Ton Silt u. Qz- Glauconit-Körner sehr
untergeordnet
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Carbonate Reef
Mixed Sample:
Carbonat > Ton/Silt/
Sand/Kies
2015-AltT1
1250
1250
Sample
(cuttings)
Cuttings: wieß, dunkelgraue Stücke, <0,5cm, kugelig
Lithologie: Karbonate überwiegen, daneben Ton/Sand u. Qz/Glaukonit-
Körner
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Carbonate Reef
Mixed Sample:
Carbonat > Ton/Silt/
Sand/Kies
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxviii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-AltT1 580 580
Sample
(cuttings)
Cuttings: hellgrau, 0,5cm-3cm, plattig bis kugelig
Lithologie: Tonklasten mit Silt/Feinsandüberzug u. wenige Siltig/sandige
Klasten
Verunreinigung: wenig Bauschutt?
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt/Sand
2015-AltT1 620 620
Sample
(cuttings)
Cuttings: mittelgrau, mm-2cm groß, plattig bis eckig, verklumpend
Lithologie: Ton > Silt, Sand
Verunreinigung: Bauschutt
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt/Sand
2015-AltT1 640 640
Sample
(cuttings)
Cuttings: mittelgrau, mm-5cm, kugelig bis eckig, stark verklumpend
Lithologie: Drill Gouge?
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt)
2015-AltT1 650 650
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm, meist kugelig
Lithologie: Tonklasten, Silt/Sand untergeordnet
Verunreinigung: Bauschutt
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt/Sand
2015-AltT1 670 670
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm, plattig bis kugelig, absandend, wenig
Material
Lithologie: FS/Silt
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-AltT1 690 690
Sample
(cuttings)
Cuttings: hellgrau, 0,5-3cm, plattig-kugelig
Lithologie: Ton
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt
2015-AltT1 700 700
Sample
(cuttings)
Cuttings: mittelgrau, 1-4cm groß, kugelig
Lithologie: Ton
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt
2015-AltT1 720 720
Sample
(cuttings)
Cuttings: hellgrau, mm-3cm, plattig bis kugelig,
Lithologie: alles dabei
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-AltT1 740 740
Sample
(cuttings)
Cuttings: hellgrau, 1-3cm, kugelig
Lithologie: Tonkugeln, 1 Sandkugel
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt/Sand
2015-AltT1 760 760
Sample
(cuttings)
Cuttings: hellgrau, 1-3cm, plattig bis kugelig
Lithologie: Tonklasten mit Siltüberzug
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton >
Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxix
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-AltT1 780 780
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm, plattig bis kugelig, leicht verklumpend
Lithologie: Tonklasten mit Siltüberzug
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton/Silt
2015-AltT1 830 830
Sample
(cuttings)
Cuttings: hellgrau, mm-4cm, plattig bis kugelig verklumpend, absandend
Lithologie: Tonklasten mit Silt u. Sandüberzug, Sand dazwischen
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt/
Sand
2015-AltT1 850 850
Sample
(cuttings)
Cuttings: mittelgrau, mm-5cm, plattig, eckig, stark verklumpend
Lithologie: Silt, Ton, VFS
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt > Ton
2015-AltT1 870 870
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm, meist plattig, verklumpend
Lithologie: Tonstücke mit Siltüberzug, Feinsand, verkittete Mineralkörner
Verunreinigung: Bauschutt,
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-AltT1 920 920
Sample
(cuttings)
Cuttings: mittelgrau, mm-2cm, plattig, kugelig verklumpend
Lithologie: Vorwiegend Fein/Grobsand
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample: Sand >
Ton/Silt
2015-AltT1 940 940
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm groß, kugelig bis eckig, absandend
Lithologie: Feinsand, einzelne Mineralkörner
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample:
VFSand/Silt > Sand
2015-AltT1 970 970
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1cm, plattig u. kugelig, wenig Material
Lithologie: Tonstücke mt Siltüberzug, einzelne verkittete Mineralkörner
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt
> Feinkies
2015-AltT1 990 990
Sample
(cuttings)
Cuttings: dunkelgrau, 1-3cm, gut gerundet kugelig
Lithologie: Tonkugeln, einzelne Qz-Körner verkittet, wenige CO3
zementierte Sandstücke
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt
> Feinkies
2015-Mail2
1000
1000
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm, plattig, kugelig, verklumpend
Lithologie: glimmereiche Feinsande u. Silte, wenig Ton
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2
1030
1030
Sample
(cuttings)
Cuttings: grau, leicht gelblich, mm-2cm verklumpend, sonst kugelig bis
plattig
Lithologie: Ton Silt Feinsand verklumpend
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt/
VFSand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxx
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Mail2
1060
1060
Sample
(cuttings)
Cuttings: hellgrau, absandend und cm groß verklumpend
Lithologie: VFS-Silt-Klumpen, absandend
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
Drillgouge (VFS/Silt)
2015-Mail2
1090
1090
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm groß, plattig bis kugelig, absandend
Lithologie: Feinsand, glimmerreich
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2
1125
1125
Sample
(cuttings)
Cuttings: mittelgrau, mm-1cm groß, plattig elongiert, selten kugelig
Lithologie: Ton u. Siltklasten, wenig gröberes
Verunreinigung: Pflanzenreste, Bauschuttreste?
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-Mail2
1145
145
Sample
(cuttings)
Cuttings: dunbkelbraun, mm-1cm groß, meist plattig, seltener kugelig
Lithologie: Tonklasten mit "erdigem" Überzug
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Mail2
1165
1165
Sample
(cuttings)
Cuttings: dunbkelbraun, m-1cm groß, klein plattig und größer kugelig
verklumpend
Lithologie: Tonklasten mit "erdigem" Überzug
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Mail2
1175
1175
Sample
(cuttings)
Cuttings: mittelgrau, mm-2cm groß, klein plattig bis größer kugelig, erig
Lithologie: Tonklasten mit erdigem Überzug
Verunreinigung: wenige Pflanzenreste
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Mail2
1190
1190
Sample
(cuttings)
Cuttings: dunkelgraubraun, mm-1cm groß, klein plattig und größer
kugelig, sehr wenig Material
Lithologie: ton-Siltklasten mit erdigem Überzug
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Mail2
1220
1220
Sample
(cuttings)
Cuttings: dunkelgraubraun, mm-1cm groß, klein plattig und größer
kugelig, sehr wenig Material
Lithologie: ton-Siltklasten mit erdigem Überzug
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Wildendürnbach
Formation
Mixed Sample: Ton >
Silt
2015-Mail2
1240
1240
Sample
(cuttings)
Cuttings: sehr dunkelgrau bis dunkelbraun, mm große Blättchen und
größere Klumpen, sehr wenig Material
Lithologie: Ton mit erdigem Überzug
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Bioturbated
Sandstone
Mixed Sample: Ton >
Silt
2015-Mail2
1250
1250
Sample
(cuttings)
Cuttings: dunkelgrau-bräunlich, mm-1cm groß, kugelig-plattig, "erdig",
verklumpend
Lithologie: erdig überzogene Ton u. Siltklasten
Verunreinigung: viele Pflanzenreste, wenige magnetische Stücke
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Bioturbated
Sandstone
Mixed Sample: Ton/Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxi
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Mail2
1260
1260
Sample
(cuttings)
Cuttings: bräunlich-dunkelgrau, mm-< 1cm, plattig, selten kugelig,
verklumpend, wirkt "erdig" ungewaschen, wenig Material
Lithologie: Silt u. Tonstücke mit erdigem überzug
Verunreinigung: Pflanzenreste
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Bioturbated
Sandstone
Mixed Sample: Ton/Silt
2015-Mail2
1280
1280
Sample
(cuttings)
Cuttings: dunkelgrau, mm-2cm groß, plattig, wenig Material
Lithologie: Tonblättchen, seltener Silt, CO3 zementierte Sandstücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample: Ton >
Silt/Sand
2015-Mail2
1310
1310
Sample
(cuttings)
Cuttings: dunkelgrau, mm-1,5cm, meist plattig, absandend erdig
Lithologie: Ton mit "erdigem" Überzug
Verunreinigung: wenige Pflanzenreste, wenige magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample: Ton >
Silt
2015-Mail2
1342,5
1345
Sample
(cuttings)
Cuttings: mittelgrau, mm groß, kugelig, selten plattig
Lithologie: Qz-reicher Grobsand, CO3 zementoierter Sand u. Silt-Ton-
Stücke
Verunreinigung: Planzenreste, magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample: Feinkies
/Grobsand> Ton/Silt
2015-Mail2
1365
1365
Sample
(cuttings)
Cuttings: farblos-hellgrau, mm groß, kugelig
Lithologie: Qz-reicher Grobsand
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample:
Feinkies/Sand
2015-Mail2
1400
1400
Sample
(cuttings)
Cuttings: mittelgrau-grünlich-farblos, mm groß, kugelig,
Lithologie: Grobsand-Feinkies, Qz-reich, Glaukonit?, CO3 zementierte
Sande
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample:
Feinkies/Sand
2015-Mail2
1435
1435
Sample
(cuttings)
Cuttings: grau bis speckig, mm-1cm, große plattige u. kleine kugelige
Stücke, sehr wenig Material
Lithologie: große flache Tonstücke, mm-großer Qz-Kies, CO3 zementierte
Sande
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Mixed Sample: Feinkies
/Grobsand> Sand/Silt/
Ton
2015-Mail2
1470
1470
Sample
(cuttings)
Cuttings: weiß, mm-1cm , plattig bis kugelig, stark absandend
Lithologie: Karbonate
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Carbonate Reef
Carbonate
2015-Mail2
1500
1500
Sample
(cuttings)
Cuttings: weiß, mm-1cm groß, kugelig bis plattig, wenig Material
Lithologie: Karbonat
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Carbonate Reef
Carbonate
2015-Mail2 570 570
Sample
(cuttings)
Cuttings: mittelgrau, mm-3cm, verklumpend, eckig
Lithologie: ?
Verunreinigung: keine
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Mail2 590 590
Sample
(cuttings)
Cuttings: mittelgrau, mm-3cm, verklumpend, eckig
Lithologie: ?
Verunreinigung: keine
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
2015-Mail2 620 620
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm, kugelig bis plattig, verklumpend
Lithologie: glimmereiche Silte u. Feinsande
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2 675 675
Sample
(cuttings)
Cuttings: hellgrau, 0,5-3cm groß, plattig bis kugelig, verklumpend
Lithologie: Ton u. Siltklasten
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample: Ton/Silt
2015-Mail2 700 700
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm groß, plattig bis kugelig verklumpend
Lithologie: glimmerreiche Silte u. Feinsande, wenig Tonklasten
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2 730 730
Sample
(cuttings)
Cuttings: hellgrau, mm-1,5cm groß, kugelig bis plattig
Lithologie: glimmereicher Feinsand u. Silt, wenig Tonklasten, wenige
Einzelmineralkörner
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2 790 790
Sample
(cuttings)
Cuttings: hellgrau, leicht gelblich, mm-1cm, plattig bis kugelig,
verklumpend
Lithologie: glimmerreiche Silte u. Feinsande, wenig Tone
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-Mail2 825 825
Sample
(cuttings)
Cuttings: mittelgrau, 0,2cm-1,5cm, leicht geplättet bis kugelig
Lithologie: Tonklasten mitSiltüberzug, glimmerführend
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample: Ton >
Silt/Sand
2015-Mail2 845 845
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm groß, meist kugelig, absandend
Lithologie: Tonklasten, mit Feinsand-Überzug, Silt u. glimmereicher VFS
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample: Ton/Silt/
VFSand
2015-Mail2 870 870
Sample
(cuttings)
Cuttings: hellgrau, mm-2cm, kugelig bis plattig, verklumpend, absandend
Lithologie: glimmereicher Feinsand, wenig Tonklasten oder Qz-
Einzelkörner
Verunreinigung: kein
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Sand/Ton
2015-Mail2 900 900
Sample
(cuttings)
Cuttings: bunt (grau, gelblich, farblos, weiß), mm-1cm, kugelig
Lithologie: Qz-reicher Feinkies, Grobsand, eckige Silt u. Tonklasten
Verunreinigung: keine
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample: Feinkies
/Grobsand> Sand/Silt/
Ton
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxiii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Mail2 920 920
Sample
(cuttings)
Cuttings: hellgrau, sub mm bis 2cm, kugelig, selten plattig, verklumpend,
absandend, teils eckig
Lithologie: glimmereiche Feinsande, wenige Qz-reiche Grobsande, wenig
Ton
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Sand/Ton
2015-Mail2 945 945
Sample
(cuttings)
Cuttings: hellgrau, mm-3cm groß, plattig bis kugelig stark verklumpend,
absandend
Lithologie: glimmereiche Silte/Feinsande, wenig Tone
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Mixed Sample:
VFSand/Silt > Ton
2015-AltT1 560 560
Sample
(cuttings)
Cuttings: mittelgrau, 0,5cm-3cm, kugelig bis plattig
Lithologie: Ton/Silt
Verunreinigung: wenig Bauschutt
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mixed Sample: Ton/Silt
2014-Mail2
1114,5_1-0,5
1114.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Sand
2014-Mail2
1114,5_0,5-0,25 1114.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Sand
2014-Mail2
1114,5_<0,25
1114.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Transition Facies
Ottnangian/
Karpatian
Sand
2014-Mail2 653
2-1mm
653
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 653
1-0,5mm
653
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 653
0,5-0,25mm
653
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 653
0,25-0,063mm
653
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Mail2 651
>2mm
651
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Conglomerate, Fine
grained Gravel
2014-Mail2 554
sand
554
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
Sand
2014-Laa1
1796,5 Mud
1796.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-Laa1
1795,3 Mud
1795.3
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-Laa1
1795,3 Sand
1795.3
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxiv
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Laa1
1635,5 Sand
1635.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Sand
2014-Laa1
1635,5 Mud
1635.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-Laa1
1633,7 Sand
1633.7
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Sand
2014-Laa1
1633,7 Mud
1633.7
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Mud
2014-AltT1
1205 Oben Sand 1205
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Bioturbated
Sandstone
Sand
2014-AltT1
1205 Unten
Sand
1205
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Carbonate Reef
Sand
2014-Mail2
1381 Sand
1381
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Basal External
Sands
Sand
2014-AltT1
1001,5 Sand
1001.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Traisen Formation Sand
2014-AltT1
801,4 VFS
801.4
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Transition Facies
Ottnangian/
Karpatian
Very fine grained Sand,
Sand
2014-AltT1
504,5 Mud
504.5
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
Mud
2015-01/01 V
no CO3
0
Sample
1 -
-
-
-
-
-
- 1 -
- Zellersteritzen
15.26445371
47.68721238
Augenstein
Formation
unknown
2015-01/03 I
1-0,5 mm no
CO3
0
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Mailberg
15.26225971
47.68814417
Augenstein
Formation
unknown
2014-Laa1 1797
Sand
1797
Sample
1 -
-
-
-
-
-
- 1 -
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
Sand
2015-Por2 1015 1015
Sample
(cuttings)
Cuttings: mittelgrau, mm-cm große Blättchen
Lithologie: Ton/Silt Blättchen, vereinzelte Qz-Körner
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton >
Silt
2015-Por2 1035 1035
Sample
(cuttings)
Cuttings: hellgrau, mm groß kugelig und mm-cm große Blättchen
Lithologie: Ton, silt, karbonatisch zementierter Sand u. quarzitischer
Feinkies
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 1060 1060
Sample
(cuttings)
Cuttings: helle (Qz) u. dunkle Körner, mm groß, kugelig
Lithologie: quarzitischer Feinkies, wenige Ton-Stücke
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Feinkies
/Grobsand> Ton/Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxv
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Por2 1095 1095
Sample
(cuttings)
Cuttings: hellgrau, mm groß, kugelig, wenige größere Blättchen
Lithologie: quarzitischer Feinkies, untergeordnet auch karbonatisch
zementierter Sand (+ dunkle mineralkörner), Ton u. Siltblättchen
Verunreinigung: magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Feinkies
/Grobsand> Sand/Silt/
Ton
2015-Por2 1125 1125
Sample
(cuttings)
Cuttings: mittelgrau, mm-cm große Blättchen, teils elongiert
Lithologie: Ton/Silt Blättchen
Verunreinigung: sehr wenige magnetische Stücke
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Por2 1145 1145
Sample
(cuttings)
Cuttings: hellgrau, mm-cm große Blättchen sowie größere Kugeln
Lithologie: Tonblättchen u. CO3 haltige siltige Kugeln
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Por2 1165 1165
Sample
(cuttings)
Cuttings: mittelgrau, mm-cm große Blättchen, auch elongiert
Lithologie: Ton/Silt Stücke, wenige Feinsandstücke oder einzelne Qz-
Körner
Verunreinigung: mini-Eisendraht; wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Por2 1175 1175
Sample
(cuttings)
Cuttings: hellgrau, mm-cm große Blättchen, cm große sehr helle Kugeln
Lithologie: To/Silt-Blättchen sowie cm große CO3 reiche siltige
Kügelchen
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Robulus Schlier
Mixed Sample: Ton >
Silt
2015-Por2 1195 1195
Sample
(cuttings)
Cuttings: bunt (dunkel-hellgrau, gelb, weiß); mm-groß kugelig, wenige
größere Blättchen
Lithologie: bunter mix, Qz u. Fsp-Feinkies, Sandstücke, Ton/Silt-Stücke
Verunreinigung: sehr viele magnetische Stücke
Qualität 1-5: 5 (geringe Probenmenge)
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Robulus Schlier
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 1220 1220
Sample
(cuttings)
Cuttings: dunkelgrau, mm-cm große Blättchen, wenige hellere
GrobsiltKlumpen
Lithologie: überwiegend Ton, wenig Silt
Verunreinigung: ganz wenig magnetische Stücke
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Mixed Sample: Ton >
Silt
2015-Por2 1250 1250
Sample
(cuttings)
Cuttings: mittelgrau, mm-cm große Blättchen, oft elongiert
Lithologie: Ton-Stücke, wenig Silt
Verunreinigung: kaum magnetische Stücke
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Mixed Sample: Ton >
Silt
2015-Por2 1270 1270
Sample
(cuttings)
Cuttings: hellgrau-gelblich, mm-groß kugelig, wenige größere Blättchen
Lithologie: quarzitischer Feinkies, wenige To-Silt-Blättchen
Verunreinigung: Holzstücke, viele magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Mixed Sample: Feinkies
/Grobsand> Ton/Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxvi
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Por2 1290 1290
Sample
(cuttings)
Cuttings: mittelgrau, mm-cm-groß, Blättchen
Lithologie: Ton u. Silt (glimmerig?); wenig quarzitischer Feinkies
Verunreinigung: magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Bioturbated
Sandstone
Mixed Sample: Ton/Silt
> Feinkies
2015-Por2 1310 1310
Sample
(cuttings)
Cuttings: hellgrau-gelblich; mm-groß, kugelig, wenige cm-große Blättchen
Lithologie: quarzitischer Feinkies mit wenigen kaolinitschen Fsp Stücken,
einige Ton/Silt-Blättchen
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Mixed Sample: Feinkies
/Grobsand> Ton/Silt
2015-Por2 1335 1335
Sample
(cuttings)
Cuttings: mittelgrau, mm-groß, blättrig u. kugelig
Lithologie: Ton/Silt Stücke + quarzitischer Feinkies, ca. 50:50
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Mixed Sample: Ton/Silt
= Feinkies
2015-Por2 1350 1350
Sample
(cuttings)
Cuttings: hellgrau, mm-groß, kugelig
Lithologie: quarzitischer Kies u. Qz-reiche Sandstücke, Sandstücke
enthalten deutlichen Anteil an dunklen Mineralen
Verunreinigung: viele Magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Mixed Sample:
Feinkies/Sand
2015-Por2 1375 1375
Sample
(cuttings)
Größe der Cuttings: bunter mix, weiße, gelbliche, mittelgraue Stücke; mm
große Kugeln, wenige cm große elongierte Blättchen
Lithologie: Ton, Silt, Sand und quarzitischer Finkies, auch Fsp-Stücke
(Kaolinit?)
Verunreinigung: viele magnetische Stücke
Qualitä
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 1395 1395
Sample
(cuttings)
Größe der Cuttings: hellgrau-gelblich, mm-kugelig, wenige cm-große
Blättchen
Lithologie: quarzitischer Feinkies, dazu wenige Ton/Silt-Blättchen
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Fine grained Gravel
2015-Por2 1410 1410
Sample
(cuttings)
Größe der Cuttings: mittelgrau, teilweise elongierte bis 1cm große
Blättchen und runde mm große Körner
Lithologie: Ton u. Silt-Stücke, Sand, Feinkies (Qz Körner), Fein-Grob ca.
50:50
Verunreinigung: bunte Plastikstücke, Holzreste, sehr viele magnetische S
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Clay, Fine grained
Gravel, Silt, Sand
2015-Por2 1415 1415
Sample
(cuttings)
Größe der Cuttings: hellgrau, 2-5 mm groß, kugelig
Lithologie: Feinkies, runde Qz-Körner, eckige Fsp-Stücke (kaolinitisiert?);
wenige Silt-Stücke
Verunreinigung: körner oberflächlich sehr dreckig, wenige magnetische
Stücke
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Basal External
Sands
Fine grained Gravel
2015-Por2 1430 1430
Sample
(cuttings)
Größe der Cuttings: hellgrau, 2-5 mm kugelig
Lithologie: Feinkies, viele Qz Körner und (kaolinitisierte?) Fsp-Stücke,
kristalliner Kies, Kohelstücke, wenige Ton u. Silt-Stücke
Verunreinigung: viele magnetische Stücke, keine Eisenspäne?
Qualität 1-5: 2
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Fine grained Gravel
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxvii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Por2 1453 1453
Sample
(cuttings)
Größe der Cuttings: mittelgrau bis dunkelgrau, mm, wenige cm große
Stücke
Lithologie: Tone, Silte, Sande und Feinkies-Stücke
Verunreinigung: magnetische Stücke
Qualität 1-5: 4 (bunter Mischmasch)
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud, Sand
2015-Por2 1473 1473
Sample
(cuttings)
Größe der Cuttings: dunkelgrau, mm-cm große Stücke
Lithologie: Tone bis Sande, Kristallinstücke??
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Sand, Mud
2015-Por2 1483 1483
Sample
(cuttings)
Größe der Cuttings: mittelgrau-dunkelgrau, mm-cm große Blättchen
Korngröße: Tone u. Silte, wenige Sandstücke und vereinzelt monomin.
Kiesstücke
Lithologie: Tone u. Silte
Verunreinigung: Pflanzenreste, viele magnetische Stücke
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud
2015-Por2 1487 1487
Sample
(cuttings)
Größe der Cuttings: mittelgrau, mehrere mm -cm groß
Korngröße: Überwiegent Ton, daneben Silt u. einzelne Feinkieskörner
Lithologie: Tone, Silte
Verunreinigung: Holzstücke, magnetische Stücke
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud, Coal
2015-Por2 1499 1499
Sample
(cuttings)
Größe der Cuttings: mittelgrau, mm-cm große Cuttings
Korngröße: Ton, Silt, Sand u. Feinkies
Lithologie: Tone, Silte und Qz/Fsp Körner
Verunreinigung: wenige Pflanzenstücke; einige Eisenspäne
Qualität 1-5: 4 (sehr bunt gemischt)
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud, Fine
grained Gravel
2015-Por2 1510 1510
Sample
(cuttings)
Größe der Cuttings: mm-cm große, dunkle, teilweise elongierte Blättchen
Korngröße: Ton und Silt, wenige Stücke Feinsand, mm große Qz Körner
Lithologie: Tone und Silte
Verunreinigung: wenige Pflanzenstücke, einige magnetische Stücke
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud
2015-Por2 1516 1516
Sample
(cuttings)
Größe der Cuttings: mm-cm große Blättchen
Korngröße: Ton und Silt, wenig Sand
Lithologie: Ton und Silt > 90%
Verunreinigung: wenige helle Körner, einige Eisenspäne
Qualität 1-5: 3
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Upper Quartz
Arenite Series
Clay, Silt, Mud, Sand
2015-Por2 490
490
Sample
(cuttings)
Cuttings: weiß, hellgrau, mm-cm groß blättrig, flach, selten kugelig
Lithologie: Ton/Silt, Karbonat, wenige Kiesstücke
Verunreinigung: 2
Qualität 1-5: 2
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Carbonat > Ton/Silt
2015-Por2 520
520
Sample
(cuttings)
Cuttings: hell, 0,5-3cm groß u. flach, einige dunkelgraue Stücke, wenig
Material
Lithologie: Carbonate u. einige Kohlestücke
Verunreinigung:
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Carbonat > Kohle
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxviii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Por2 540
540
Sample
(cuttings)
Cuttings: weißlich, 0,5-3cm große flache Stücke
Lithologie: Carbonat?
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Carbonate
2015-Por2 570
570
Sample
(cuttings)
Cuttings: gelblich hellgrau, cm große flache u. kugelige Stücke, wenig
Material
Lithologie: Ton/Silt
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample: Ton >
Silt
2015-Por2 590
590
Sample
(cuttings)
Cuttings: hellgrau, mm-cm blättrig bis kugelig, sehr wenig Material
Lithologie: Ton/Silt, Drill Gouge?
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-Por2 610
610
Sample
(cuttings)
Cuttings: hellgrau, cm groß blättrig-kugelig, wenig Material
Lithologie: Ton/Silt
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample: Ton >
Silt
2015-Por2 640
640
Sample
(cuttings)
Cuttings: hellgrau, große Stücke (blättchen + Drill Gouge) und kugeliger
Kies, Feinstkörniges, sehr wenig Material
Lithologie: Drill Gouge (Ton-Kies)
Verunreinigung: keine
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
2015-Por2 670
670
Sample
(cuttings)
Cuttings: hellgrau bis farblos, mm kugelig, wenige größere Blättchen
Lithologie: quarzitischer Feinkies (auch andere Min), wenig
karbonatzementierter Sand, Wenige Ton/Silt-Stücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample: Feinkies
/Grobsand> Sand/Silt/
Ton
2015-Por2 710
710
Sample
(cuttings)
Cuttings: hellgrau, mm groß blättrig u. kugelig, bis 1cm große Drill Gouge
Stücke, wenig Material
Lithologie: Drillgouge (Ton-Feinkies) + Ton-Kies
Verunreinigung: Holzreste, wenige Eisenstücke
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Drillgouge + Ton-Kies
2015-Por2 740
740
Sample
(cuttings)
Cuttings: hellgrau, mm große Blättchen, Drillgouge, sehr wenig Material
Lithologie: Drillgouge (Ton/Silt)
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt)
2015-Por2 750
750
Sample
(cuttings)
Cuttings: hellgrau, cm große Drill-Gouge Stücke, wenig Material
Lithologie: Drillgouge, Ton/Silt überwiegen
Verunreinigung: keine
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
Mixed Sample:
Drillgouge (Ton/Silt)
2015-Por2 760
760
Sample
(cuttings)
Cuttings: hellgrau, mm große Blättchen, drillgouge artige Stücke, extrem
wenig Material
Lithologie: Ton-Feinkies, Drillgouge
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xxxix
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Por2 780
780
Sample
(cuttings)
Cuttings: hellgrau, mm große Blättchen, drillgouge artige Stücke, extrem
wenig Material
Lithologie: Ton-Feinkies, Drillgouge
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
2015-Por2 810
810
Sample
(cuttings)
Cuttings: hellgrau, Drillgouge?, wenige Blättchen, geringe Probenmenge
Lithologie: Ton-Feinkies scheint durch carbonatischen Zement zu
Drillgouge verkittet
Verunreinigung: Eisenkugel, wenige magnetische Stücke
Qualität 1-5: 5
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample:
Drillgouge (Ton/Silt/
Sand/Feinkies)
2015-Por2 830
830
Sample
(cuttings)
Cuttings: hellgrau, mm-cm Blättchen, mm-cm kugelig, sehr wenig
Material
Lithologie: Ton, Silt, Sand, Feinkies
Verunreinigung: fast keine
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 870
870
Sample
(cuttings)
Cuttings: bunt (hellgrau, weiß, transparent, gelblich), mm groß kugelig u.
bis cm große Blättchen, geringe Probenmenge
Lithologie: Feinkiese (Qz, Karbonate, Fsp), untergeordnet Tone/Silte
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Feinkies
/Grobsand> Sand/Silt/
Ton
2015-Por2 880
880
Sample
(cuttings)
Cuttings: hellgrau, mm-cm große Blättchen, geringe Probenmenge
Lithologie: karbonatzementierter Feinsand, wenig Silt/Ton oder Feinkies
Verunreinigung: wenige magnetische Stücke
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Sand >
Ton/Silt/Feinkies
2015-Por2 900
900
Sample
(cuttings)
Cuttings: hellgrau, eher Blättchen, sehr wenig Material
Lithologie: Ton/Silt vorherrschend
Verunreinigung: keine
Qualität 1-5: 5
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt
> Sand/Feinkies
2015-Por2 940
940
Sample
(cuttings)
Cuttings: hellgrau, mm groß kugelig, mm-cm große Blättchen
Lithologie: Viel quarzitischer Feinkies u. Karbonatzementierter Sand, auch
Ton u. Silt
Verunreinigung: magnetische Stücke
Qualität 1-5: 4
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 980
980
Sample
(cuttings)
Cuttings: hellgrau, mm groß kugelig, mm-cm große Blättchen
Lithologie: Ton, Silt, karbonat-zementierter sand u. quarzitischer Feinkies
Verunreinigung: viele magnetische Stücke
Qualität 1-5: 4
1 -
-
- 1 -
-
- 1 -
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Traisen Formation
(turbiditic)
Mixed Sample: Ton/Silt/
Sand/Feinkies
2015-Por2 490
Carbonate
490
Sample
(cuttings)
Cuttings: weiß, hellgrau, mm-cm groß blättrig, flach, selten kugelig
Lithologie: Ton/Silt, Karbonat, wenige Kiesstücke
Verunreinigung: 2
Qualität 1-5: 2
-
-
-
- 1 -
-
-
-
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2015-AltT1
1170
1170
Sample
(cuttings)
Cuttings: hellgrau mm-1c groß, meist kugelig
Lithologie: Silt/Feinsand, glimmerreich
Verunreinigung: keine
Qualität 1-5: 1
1 -
-
-
-
-
-
- 1 -
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Bioturbated
Sandstone
Mixed Sample:
VFSand/Silt
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xl
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Schb
130,8
130.8
Sample
Verwittertes Kristallines Basement
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Crystalline
Gneiss
2014-Schb 135
135
Sample
Kristallines Basement
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Crystalline
Gneiss
2014-Schb 45
45
Sample
sandiger Ton
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Mixed Sample: Ton/Silt
2014-Schb 60
60
Sample
toniger Silt, Feinsandlagen
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Mixed Sample: Ton/Silt
2014-Schb 68,5 68.5
Sample
Ton, gipsblüten
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Clay
2014-Schb 70
70
Sample
dunkler vertrockneter Ton mit Gipsblüten
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Traisen Formation Clay
2014-Schb 76
76
Sample
Dunkler Ton
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Clay
2014-Schb 95
95
Sample
Blaugrauer Ton
1 -
-
-
-
-
-
- 1 -
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
Clay
2015-Strth 1
1022,6
1022.6
Sample
dunkler mergeliger siltiger Tonstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
silty marly Claystone
2015-Strth 1
1025
1025
Sample
Sandreichere Lagen in Tonstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Fine grained Sandstone
2015-Strth 1
1051,8
1051.8
Sample
mergeliger Tonstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
marly Claystone
2015-Strth 1
1084
1084
Sample
feinkörnige hellgraue Sandsteinhorizont in Tonmergeln
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
unknown
2015-Strth 1
1084,8
1084.8
Sample
sandiger siltiger dunkler Tonmergelstein, Fossilreste, Pflanzenreste
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Silty Claystone, Fine
grained Sandstone
2015-Strth 1
1119,7
1119.7
Sample
CO3 reicher sehr feinkörniger Sandstein mit gröberen Nestern, stark
bioturbiert
1 - 3 1 1 - 1 - 1 1 -
15.95194574
48.27448633
Streithofen 1
Bioturbated
Sandstone
Very fine grained
Sandstone
2015-Strth 1
1142
1142
Sample
graublauer wenig tektonisch zerscherter Sandstein, eingeschwemmte
Pflanzenreste
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Fine grained Sandstone
2015-Strth 1
1144,8
1144.8
Sample
schwarzer tektonisch zerscherter Siltstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Siltstone
2015-Strth 1
1172,5
1172.5
Sample
dunkler feinkörniger Sandstein, pyritisierungen, Glaukonit?
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Fine grained Sandstone
2015-Strth 1
1176
1176
Sample
dunkler bioturbater mittelkörniger Sandstein mit vielen hellen Klasten,
Tonklasten, Pyritkonkretionen, viele grünliche Minerale: Glauconit?
1 -
-
-
-
- 1 - 1 - 6
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Medium Grained
Sandstone
2015-Strth 1
1178,9
1178.9
Sample
CO3 zementierter feinkörniger Sandstein
1 - 3 1 -
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Fine grained Sandstone
2015-Strth 1
1201,5
1201.5
Sample
hellgrauer mittelkörniger Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Medium Grained
Sandstone
2015-Strth 1
1202
1202
Sample
schwarzer tektonischer sandiger Siltstein mit großen Komponenten
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Sandy Siltstone
2015-Strth 1
1210,8
1210.8
Sample
grauer tektonisch zerscherter Tonstein/Siltstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Silty Claystone
2015-Strth 1
1211,5
1211.5
Sample
schwarzer tektonischer Sandstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Claystone
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xli
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Strth 1
1215
1215
Sample
schwarzer tektonischer Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Fine grained Sandstone
2015-Strth 1
1218,4
1218.4
Sample
schwarzer Sandstein, Tektonit
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Medium Grained
Sandstone
2015-Strth 1
1220
1220
Sample
weißlicher MS
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Basal External
Sands
Coarse Grained
Sandstone
2015-Strth 1
1233
1233
Sample
Dioritgneis
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Crystalline
Dioritegneis
2015-Strth 1
151,5
151.5
Sample
siltführender Tonstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
153,5
153.5
Sample
mittelkörniger Sand
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained Sand
2015-Strth 1
248,5 CS
248.5
Sample
hellgrauer grobkörniger Sand
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Coarse Grained Sand
2015-Strth 1
249,3
249.3
Sample
Ton + Sandlagen
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
301,8
301.8
Sample
Tonstein/sandig
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
303,5
303.5
Sample
grobkörniger Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Coarse Grained Sand
2015-Strth 1
351,2
351.2
Sample
Tonstein/braun
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
352,5
352.5
Sample
mittelkörniger Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained
Sandstone
2015-Strth 1
400,2
400.2
Sample
CO3 zementierter Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained
Sandstone
2015-Strth 1
404,5
404.5
Sample
mittelkörniger Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained
Sandstone
2015-Strth 1 405 405
Sample
Sand/Ton Wechsellagerung; rip up clasts in Sand
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
450,6
450.6
Sample
grobkörniger Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Coarse Grained
Sandstone
2015-Strth 1
451,9
451.9
Sample
dunkelbrauner Ton
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
452,8
452.8
Sample
weißer FS
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Fine grained Sand
2015-Strth 1
500,5
500.5
Sample
siltiger Tonstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
504,5
504.5
Sample
grobkörniger Sand/Sandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Coarse Grained
Sandstone
2015-Strth 1 53 53
Sample
Sand
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Fine grained Sandstone
2015-Strth 1
53,8
53.8
Sample
Ton + Sandlagen
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
54,2
54.2
Sample
GR-Feinkies
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Traisen Formation Very Coarse Grained
Sand
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xlii
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Strth 1
554,5
554.5
Sample
mittelkörniger hellgrauer Sand, leicht verfestigt
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained Sand
2015-Strth 1
554,8
554.8
Sample
gelblicher Tonstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation unknown
2015-Strth 1 601 601
Sample
MS-MS-Stein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained Sand
2015-Strth 1
602,7
602.7
Sample
brauner Tonstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation unknown
2015-Strth 1
653,2
653.2
Sample
mittelkörniger Sandstein
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained
Sandstone
2015-Strth 1
654,8
654.8
Sample
brauner Tonstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation unknown
2015-Strth 1
704,5
704.5
Sample
hellgrauer feinkörniger Sandstein, Drillmud?
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Fine grained Sandstone
2015-Strth 1
751,5
751.5
Sample
Kies
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Traisen Formation Fine grained Gravel
2015-Strth 1 754 754
Sample
FS-MS
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Traisen Formation unknown
2015-Strth 1
754,5
754.5
Sample
dunkler Siltstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Siltstone, Fine grained
Sandstone
2015-Strth 1 801 801
Sample
verschiedene Sandlagen, dickste bei 801
1 - 3 1 -
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Traisen Formation Fine grained Sandstone
2015-Strth 1 802 802
Sample
CO3 armer/freier Tonstein
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Claystone
2015-Strth 1
853,8
853.8
Sample
sandiger mergeliger Tonstein, cm große Qz-Körner in Tonmatrix
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation sandy marly Claystone
2015-Strth 1
854,9
854.9
Sample
CO3 armer/freier Tonstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Traisen Formation Silty Claystone
2015-Strth 1
892,8
892.8
Sample
sandiger mergeliger Tonstein, cm große Qz-Stücke,
1 - 3 - 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
sandy marly Claystone
2015-Strth 1 893 893
Sample
hellgrau Feinsandstein-Lagen in Tonmergel
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Fine grained Sandstone
2015-Strth 1 931
Gesamt
931
Sample
fine grained sand + siltstone
1 -
-
-
-
-
-
- 1 - 6
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Silty Sandstone
2015-Strth 1 931
Sand
931
Sample
silty Sandstone
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Silty Sandstone
2015-Strth 1 931
Ton
931
Sample
Ton
1 -
-
- 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Sandy Siltstone
2015-Strth 1
964,8
964.8
Sample
mergeliger sandiger graublauer Siltstein
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
marly Claystone
2015-Strth 1
990,5
990.5
Sample
CO3 reicher feinsandiger Tonstein, Fischschuppen,
1 - 3 1 1 -
-
- 1 1 -
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
silty marly Claystone
2015-Strth 1
992,6
992.6
Sample
Sandreichere Lagen in Tonstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Robulus Schlier
Fine grained Sandstone
2015-Strth 1
248,5 FS
248.5
Sample
Mittelsandstein
1 -
-
-
-
-
-
- 1 -
-
15.95194574
48.27448633
Streithofen 1
Traisen Formation Medium Grained
Sandstone
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xliii
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2014-Schb 100
XRD (new prep)
Test1
100
Sample
grauer siltiger Mergel; Schneiden!!
Mehrere cm dicke dunkle feinkörnige (Ton-Silt) Lage unterbrochen von
mm-cm dicken gröberen hellgrauen Lagen. Die hellgrauen Lagen sind
Grobsilt-SF-Sand; eine mehrere mm dicke Lage zeigt komplexe
linsenartige Strukturen
1 -
-
-
-
-
-
-
-
- Low. A. Schaubing
15.61724925
48.2578592
Schaubing
Robulus Schlier
unknown
2014-Mail2 554
XRD (new prep)
Test1 körnig
554
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
unknown
2014-Mail2 554
XRD (new prep)
Test2 körnig
554
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
unknown
2014-Mail2 554
XRD (new prep)
Test3 körnig
554
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
unknown
2014-Mail2 554
XRD (new prep)
Test4 körnig
554
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Mailberg
16.23055478
48.66057951
Mailberg 2
Laa Formation
unknown
2014-Por2 704
XRD (new prep)
Test1
704
Sample
hellbrauner Mud
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-Por2 704
XRD (new prep)
Test2
704
Sample
hellbrauner Mud
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-Por2 704
XRD (new prep)
Test3
704
Sample
hellbrauner Mud
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-Por2 704
XRD (new prep)
Test4
704
Sample
hellbrauner Mud
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.18936668
48.55780493
Porrau2
Laa Formation
unknown
2014-AltT1
504,5 XRD
(new prep) Test1
504.5
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
unknown
2014-AltT1
504,5 XRD
(new prep) Test2
504.5
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
unknown
2014-AltT1
504,5 XRD
(new prep) Test3
504.5
Sample
1 -
-
-
-
-
-
-
-
- Low.A. Altenmarkt
T1
16.23276131
48.58340218
Altenmarkt
Thermal Süd 1
Laa Formation
unknown
2015-Laa1 1750
XRD
(Instrument
Bias) Test1
1750
Sample
(cuttings)
Größe der Cuttings: mm-cm große elongierte Plättchen und kugelige
Klumpen
Korngröße: sand bis ton
Lithologie: Ton-Chips und Feinsand-Stücke, Kohlestücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xliv
PALZER-KHOMENKO, WAGREICH, KNIERZINGER, MESZAR, GIER, KALLANXHI and SOLIMAN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
2015-Laa1 1750
XRD
(Instrument
Bias) Test2
1750
Sample
(cuttings)
Größe der Cuttings: mm-cm große elongierte Plättchen und kugelige
Klumpen
Korngröße: sand bis ton
Lithologie: Ton-Chips und Feinsand-Stücke, Kohlestücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2015-Laa1 1750
XRD
(Instrument
Bias) Test3
1750
Sample
(cuttings)
Größe der Cuttings: mm-cm große elongierte Plättchen und kugelige
Klumpen
Korngröße: sand bis ton
Lithologie: Ton-Chips und Feinsand-Stücke, Kohlestücke
Verunreinigung: keine
Qualität 1-5: 3
1 -
-
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1795,8 XRD
(new prep) Test1
1795.8
Sample
Mud und helle Linsen
1 -
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1795,8 XRD
(new prep) Test2
1795.8
Sample
Mud und helle Linsen
1 -
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1795,8 XRD
(new prep) Test3
1795.8
Sample
Mud und helle Linsen
1 -
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2014-Laa
1795,8 XRD
(new prep) Test4
1795.8
Sample
Mud und helle Linsen
1 -
-
-
-
-
-
-
-
- Low.A. Laa
16.42935529
48.70801476
LAA 001
Wildendürnbach
Formation
unknown
2016-MolMeet_
Stop3 I
0
Sample
Brünner Sande
1 6 -
-
-
-
-
- 1 -
- Boscovice Graben
16.337296
49.11369
unknown
Sand
2016-MolMeet_
Stop5 I
0
Sample
Badenische Sande des nördlichen Wiener Beckens
1 6 -
-
-
-
-
- 1 -
- Wiener Becken
16.680073
48.791029
unknown
Sand
MPK-
MOL_170101 II 0
Sample
Diatomit hell, zerfällt plattig
1 - 1 -
-
-
-
- 1 -
-
55.31064115
3.136189756
Limberg Member
Diatomite
MPK-
MOL_170101 I 0
Sample
Diatomit fein geschichtet, hell, CO3 arm
1 - 1 -
-
-
-
- 1 - 4
55.31064115
3.136189756
Limberg Member
Diatomite
MPK-
MOL_170101
III
0
Sample
Zellerndorf Formation mergeliger pelit
1 - 1 - 3 -
-
- 1 -
-
55.31064115
3.136189756
Zellerndorf
Formation
Pelite
MPK-
MOL_170101
IV
0
Sample
tephra oder Löss?
1 - 1 -
-
-
-
- 1 - 7
55.31064115
3.136189756
unknown
Tephra
MPK-
MOL_170101 V 0
Sample
Pelit oberer Teil Zellerndorf Formation?
1 - 1 - 3 -
-
- 1 - 7
55.31064115
3.136189756
unknown
unknown
MPK-
MOL_170101
VI
0
Sample
weißes Zeug in der zellerndorf Formation, Carbonat
1 - 1 - 3 -
-
- 1 -
-
55.31064115
3.136189756
Zellerndorf
Formation
Carbonate
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).
xlv
THE OTTNANGIAN CALCITE CRISIS IN THE NORTH ALPINE–CARPATHIAN FORELAND BASIN
GEOLOGICA CARPATHICA
, 2018, 69, 4, 315–334
Sample No.
Depth GOK
Sample — Kind
Description
XRD
Heavy minerals
Chemistry
Dinoflagelate cysts
Calcarfeous Nannofossils
Micr
opr
obe
Foraminifera
XRF-Pr
ofile
XRF-Bulk
Clays
Thin section
Location
WGS 84 Longitude
WGS 84 Latitude
W
ell
Formation / Lithodem
Lithology
MPK-
MOL_170101
VII
0
Sample
Konkretion, rund um Stein?
1 - 1 -
-
-
-
- 1 - 7
55.31064115
3.136189756
Zellerndorf
Formation
Concretion
MPK-
MOL_170101
VIII
0
Sample
1 - 1 - 3 -
-
1 -
-
55.31064115
3.136189756
Zellerndorf
Formation
Pelite
Legend: 1 — investigated; 2 — in investigation; 3 — sent; 4 — prepared; 5 — in preparation; 6 — planned (priority); 7 — planned (no priority).