MORPHOSTRUCTURE PATTERNS IN SATELLITE MULTISPECTRAL LANDSAT TM IMAGES
Published: Oct 1998
Pages: 307 - 313
Authors: ISSAAK PARCHARIDIS
Abstract: The possibility of tectonic observations using multispectral remote sensing data is based mainly on morphostructures, which could lead directly to the structural interpretation of the area. This work aims to contribute to the creation of a morphostructure-code with a corresponding key-legend, in order to facilitate the acquisition of tectonic information by users, who do not specialize in remote sensing. The studied area covers a great part of NW Greece (Epirus Prefecture). During the summer and autumn of 1996, this region was affected by strong and disastrous earthquakes (up to 5.6 R). Data from Landsat TM have been selected and processed creating a false colour composite image and then analyzed and interpreted in order to detect the tectonic features.
Keywords: NW Greece, Epirus, tectonism, morphostructure, Remote Sensing, Landsat
Download PDF document
Volume 49 no. 5 / October 1998
ISSAAK PARCHARIDIS
MORPHOSTRUCTURE PATTERNS IN SATELLITE MULTISPECTRAL LANDSAT TM IMAGES
RADU GIRBACEA, WOLFGANG FRISCH, HANS-GERT LINZER
POST-OROGENIC UPLIFT-INDUCED EXTENSION: A KINEMATIC MODEL FOR THE PLIOCENE TO RECENT TECTONIC EVOLUTION OF THE EASTERN CARPATHIANS (ROMANIA)
EDUARD KOSA
LITHOSTRATIGRAPHY AND DEPOSITIONAL ENVIRONMENT OF LOWER–MIDDLE JURASSIC CRINOIDAL LIMESTONE FORMATIONS OF THE VYSOKA NAPPE UNIT (MALE KARPATY MTS., WESTERN CARPATHIANS)
JAKOB PAMIC
NORTH DINARIDIC LATE CRETACEOUS-PALEOGENE SUBDUCTION-RELATED TECTONOSTRATIGRAPHIC UNITS OF THE SOUTHERN TISIA, CROATIA
NADJA OGNJANOVA-RUMENOVA, DIONYZ VASS
PALEOECOLOGY OF THE LATE MIOCENE MAAR LAKES, PODRECANY BASALT FORMATION, SOUTHERN SLOVAKIA, ON THE BASIS OF SILICEOUS MICROFOSSILS
SERGEI P. KORIKOVSKY, MARIAN JANAK, BRANISLAV LUPTAK
PHASE RELATIONS IN OLIVINE-ORTHOPYROXENE-CHLORITE-SPINEL-HORNBLENDE METAULTRAMAFICS FROM THE MALA FATRA MTS., WESTERN CARPATHIANS
MONIKA ORVOSOVA, JURAJ MAJZLAN, MARTIN CHOVAN
HYDROTHERMAL ALTERATION OF GRANITOID ROCKS AND GNEISSES IN THE DUBRAVA Sb-Au DEPOSIT, WESTERN CARPATHIANS