Contents
U-Au-Co-Bi-REE MINERALIZATION IN THE GEMERIC UNIT (WESTERN CARPATHIANS, SLOVAKIA)
Published: Oct 1997
Pages: 303 - 313
Authors: IGOR ROJKOVIC, MILAN HABER, LADISLAV NOVOTNY
Abstract: Uranium mineralization occurs in a quartz vein with gold and REE minerals. The vein cuts the Early Paleozoic rocks in the proximity of the granite body of the Humel Massif. The mineralization is represented by uraninite, brannerite, arsenopyrite, pyrite, glaucodot, gold, galena, bismuth, bismuthinite, xenotime-(Y), rutile, sericite, chlorite, apatite, monazite-(Ce) and tourmaline. Secondary minerals are represented by goethite, trögerite, zeunerite and scorodite.
Keywords: Gemeric Unit, Early Paleozoic, quartz vein, U-Au-Co-Bi-REE minerals, element association
Download PDF documentVolume 48 no. 5 / October 1997
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