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 document
Volume 48 no. 5 / October 1997
MARIAN JANAK, BRANISLAV LUPTAK
PRESSURE-TEMPERATURE CONDITIONS OF HIGH-GRADE METAMORPHISM AND MIGMATITIZATION IN THE MALA FATRA CRYSTALLINE COMPLEX, THE WESTERN CARPATHIANS
IGOR ROJKOVIC, MILAN HABER, LADISLAV NOVOTNY
U-Au-Co-Bi-REE MINERALIZATION IN THE GEMERIC UNIT (WESTERN CARPATHIANS, SLOVAKIA)
ATTILA DEMENY, ISTVAN GATTER, MIKLOS KAZMER
THE GENESIS OF MESOZOIC RED CALCITE DIKES OF THE TRANSDANUBIAN RANGE (HUNGARY): FLUID INCLUSION THERMOMETRY AND STABLE ISOTOPE COMPOSITIONS
SORIN FILIPESCU, RADU GIRBACEA
LOWER BADENIAN SEA-LEVEL DROP ON THE WESTERN BORDER OF THE TRANSYLVANIAN BASIN: FORAMINIFERAL PALEOBATHYMETRY AND STRATIGRAPHY
SALEM YASEEN MEJEED
MICROMORPHOLOGICAL STUDY OF CALCRETES IN SOILS OF THE ZITNY OSTROV REGION, SOUTHWESTERN SLOVAKIA
PETER LUPTAK
UPPER JAW FRAGMENT OF THE ANANCUS ARVERNENSIS (CROIZET & JOBERT 1828) (MASTODONTIDAE, PROBOSCIDEA, MAMMALIA) FROM THE VILLAFRANCHIAN OF HAJNACKA, SLOVAKIA