U-AU-CO-BI-REE MINERALIZATION IN THE GEMERIC UNIT (WESTERN CARPATHIANS, SLOVAKIA)

Uranium mineralization occurs in a quartz vein with gold and REE miner als. The vein cuts the Early Paleozoic rocks in the proximity of the g ranite body of the Humel Massif. The mineralization is represented by uraninite, brannerite, arsenopyrite, pyrite, glaucodot, gold, galena, bismuth, bismuthinite, xenotime-(Y), rutile, sericite, chlorite, apati te, monazite-(Ce) and tourmaline. Secondary minerals are represented b y goethite, trogerite, zeunerite and scorodite.