International Geological Journal - Official Journal of the Carpathian-Balkan Geological Association

U-Au-Co-Bi-REE MINERALIZATION IN THE GEMERIC UNIT (WESTERN CARPATHIANS, SLOVAKIA)

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

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