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Title New knowledge about U-Cu mineralization on the Kozie chrbty Mts. and its relationship to the (late Neotectonic) structures (Hronic Unit, Western Carpathians, Slovakia) Author info Eva Hoppanová ... [et al.] Author Hoppanová Eva 1995- (85%) UMBFP01 - Katedra geografie a geológie
Co-authors Ferenc Štefan 1977- (5%) UMBFP01 - Katedra geografie a geológie
Šimonová Viera 1977- (5%) UMBFP01 - Katedra geografie a geológie
Kopáčik Richard 1995- (5%) UMBFP01 - Katedra geografie a geológie
Source document 15th Emile Argand Conference on Alpine Geological Studies : 12-14 September 2022, Ljubljana, Slovenia : abstract book and fieldtrip guide. Pp. 31. - Ljubljana : University of Ljubljana, 2022 ; Emile Argand Conference on Alpine Geological Studies konferencia Keywords mineralizácia - mineralization Headings Geogr. Západné Karpaty (pohorie) Kozie chrbty Form. Descr. príspevky v zborníku - proceedings papers Language English Country Slovenia Public work category AFG No. of Archival Copy 52028 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ 
article
Title Supergénne alterácie stratiformnej U-Cu mineralizácie v mladšom paleozoiku hronika Kozích chrbtov a Nízkych Tatier Subtitle diplomová práca Author info Eva Hoppanová; školiteľ: Štefan Ferenc Author Hoppanová Eva 1995-
Another authors Ferenc Štefan 1977- (Školiteľ (konzultant))
Corporation Univerzita Mateja Bela . Fakulta prírodných vied . Katedra geografie a geológie , Banská Bystrica, Slovensko Issue data Banská Bystrica , 2020. - 88 s. Keywords uranylové minerály urán - uranium meď - copper hronikum Headings Geogr. Nízke Tatry (Slovensko : pohorie) Slovensko východné Kozie chrbty Form. Descr. diplomové práce - master’s theses Language Slovak Country Slovak Republic systematics 553.061.2 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xk - Kvalifikačné práce Copy count 1, currently available 0, at library only 1 
book
Title Kremeňovo-karbonátové žily s U-Mo-Cu mineralizáciou v permských intermediárnych až bázických vulkanitoch hronika na lokalite Kravany (Kozie chrbty, východné Slovensko) Par.title Quartz-carbonate veins containing U-Mo-Cu mineralization in the Permian intermediate to basic volcanic rocks of the Hronicum Unit at Kravany (Kozie chrbty Mts., Eastern Slovakia) Author info Štefan Ferenc, Tomáš Mikuš ... [et al.] Author Ferenc Štefan 1977- (50%) UMBFP01 - Katedra geografie a geológie
Co-authors Mikuš Tomáš (15%)
Spišiak Ján 1953- (15%) UMBFP01 - Katedra geografie a geológie
Kopáčik Richard 1995- (10%) UMBFP01 - Katedra geografie a geológie
Hoppanová Eva 1995- (10%) UMBFP01 - Katedra geografie a geológie
Source document Bulletin Mineralogie Petrologie. Roč. 28, č. 2 (2020), s. 364-384. - Praha : Mgr. Jiří Sejkora, 2020 Keywords uraninit - uraninite horniny - rocks hronikum Headings Geogr. Západné Karpaty (pohorie) Slovensko východné Kozie chrbty Form. Descr. články - journal articles Language Slovak Country Czech Republic Annotation Historical uranium ore deposit Kravany is located in the eastern part of Kozie Chrbty Mts., approximately 9 km SW of the district town Poprad. Stratiform, infiltration U-Cu-Pb mineralization is bound to the Upper Permian clastic sediments (Kravany Beds, member of Malužiná Formation, Hronicum Unit), which are enriched in fragments of carbonized flora. Vein U-Mo-Cu mineralization was found in the Upper Permian intermediate to basic volcanics intersecting the sediments of the Kravany Beds (also ore lenses). Vein filling originated in the following development stages: I.) Quartz-pyrite (quartz, pyrite, marcasite), II.) Dolomite-pyrite (dolomite, pyrite, marcasite, galena), III.) Copper (tetrahedrite, tennantite, chalcopyrite), IV.) Uranium-molybdenum (uraninite, Pb-Mo-S phase, coffinite, quartz), and V.) Calcite (calcite, chalcopyrite). The formation of mineralization can be explained by the geological position: random emplacement of the diorite porphyrites, resp. basaltoid andesites dikes, directly in the preexisting U,Mo-bearing sediments. Vein U-Mo-Cu mineralization could thus most likely have formed according to the following scenario: I.) sedimentation of Kravany Beds in the Permian riftogenic basin: formation of beds of arkoses and arkosic sandstones with abundant fragments of charred flora, II.) formation of infiltration U mineralization: reduction and accumulation of U in sediments rich in organic matter, III.) emplacement of dikes of intermediate to basic volcanics: intersection of sediments with organics and with high U and Mo content, mobilization of formation fluids, assimilation of U and Mo into intermediate-basic magma, IV.) cooling of volcanic bodies → their contraction (formation of contraction cracks) → filling of contraction cracks with quartz, carbonates and ore minerals (crystallization from residual magmatic solutions mixed with formation waters). From this point of view it is syngenetic volcanogenic vein U-Mo-Cu mineralization, originally of the Permian age, with subsequent Alpine (most probably Cretaceous) reworking (this is evidenced by the variable composition of uraninite). It belongs to the Neohercynian late- to postorogenic metallogenetic stage. The possible younger, post-Permian age of mineralization from alpine hydrothermal solutions must also be assumed, but this consideration has several inconsistencies. URL Link na plný text Public work category ADM No. of Archival Copy 49312 Repercussion category KONDELA, Julián - HREUS, Sebastián. Uranium mining restriction in Slovakia from the perspective of actual raw material situation. In International conference mineral deposits safeguarding as a basis of mineral raw materials safety : books of abstracts, Kraków, 10th-11th May 2022. Kraków : Mineral and energy economy research institute PAS, 2022. ISBN 978-83-964171-5-2, pp. 33-34.
Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika article
Title Supergénne minerály stratiformnej U-Cu mineralizácie pri Spišskej Teplici (hronikum, Kozie chrbty, východné Slovensko) Par.title Supergene minerals of stratiform U-Cu mineralization at Spišská Teplica (Hronicum Unit, Kozie chrbty Mts., Eastern Slovakia) Author info Štefan Ferenc, Eva Hoppanová ... [et al.] Author Ferenc Štefan 1977- (35%) UMBFP01 - Katedra geografie a geológie
Co-authors Hoppanová Eva 1995- (35%) UMBFP01 - Katedra geografie a geológie
Kopáčik Richard 1995- (10%) UMBFP01 - Katedra geografie a geológie
Mikuš Tomáš (10%)
Budzák Šimon 1982- (10%) UMBFP08 - Katedra chémie
Source document Bulletin Mineralogie Petrologie. Roč. 28, č. 2 (2020), s. 295-306. - Praha : Mgr. Jiří Sejkora, 2020 Keywords urán - uranium meď - copper malachite azurite Headings Geogr. Kozie chrbty Západné Karpaty (pohorie) Spiš (Slovensko : oblasť) Form. Descr. články - journal articles Language Slovak Country Czech Republic Annotation Occurrence of infiltration, stratiform U-Cu mineralization Spišská Teplica - Vápenica-Vysová is located approximately 7.8 km SW from the district town Poprad and 4.3 km SW from the centre of Spišská Teplica village (Slovak Republic). Primary U-Cu mineralization is bound to arkosic sandstones with abundant carbonised fragments of higher plants (Kravany Beds, Upper Permian, Hronicum Unit) and consists of uraninite and pyrite. The chalcopyrite and Cu-S mineral phase (digenite?, roxbyite?) form inclusions in clastic fluorapatite and zircon. From the supergene minerals, malachite and goethite are absolutely dominant, azurite, zálesíite and baryte are less represented. Phosphate, probably of the florencite group and acanthite, were only rarely found. Supergene uranyl minerals were not detected. Their lack, resp. their weak development in all uranium deposits in Kozie Chrbty Mts. can be explained as follows: during the weathering of primary ores, the cation UO22+ is released from uraninite and coffinite into supergene solutions (uranyl complexes). However, these solutions come into almost immediate contact with fragments of coalified flora (especially in the case of rich U ores), where UO22+ binds to the organic uranyl complexes (complexation). Only a relatively small part of uranyl cation escapes from this geochemical trap, and in that case supergene uranium minerals may precipitate. URL Link na zdrojový dokument Public work category ADM No. of Archival Copy 49309 Catal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Database xpca - PUBLIKAČNÁ ČINNOSŤ References PERIODIKÁ-Súborný záznam periodika article
Title Menej známe stopy medenorudného baníctva na západe Spiša Author info Štefan Ferenc, Marián Soják, Ľuboslav Maťo Author Ferenc Štefan 1977- (70%)
Co-authors Soják Marián (20%)
Maťo Ľuboslav (10%)
Source document Meď v Európe : medzinárodný seminár, Banská Štiavnica, 15. - 17. október 2003. S. 34-55. - Banská Štiavnica : Slovenské banské múzeum, Slovenská agentúra životného prostredia Banská Bystrica, 2003 / Labuda Jozef ; Šušková Helena ; Zerola Jaroslav Keywords meď - copper ťažba medi Headings Geogr. Kozie chrbty Vikartovský chrbát Spiš (Slovensko : oblasť) Language Slovak Country Slovak Republic systematics 553 Public work category AFD No. of Archival Copy 21950 Repercussion category HARNIČÁR, Adrián - MLYNARČIKOVÁ, Daniela - ROTH, Peter. Zaniknuté banské diela na hornom toku Hornádu. In Archologia technica 22: zkoumání výrobních objektů a technologií archeologickými metódami : sborník přednášek z 29. semináře Archeologia technica 29. duben 2010. Brno : Technické múzeum v Brne, 2011. ISBN 978-80-86413-78-5, s. 61-70.
HARNIČÁR, Adrián a kol. Vikartovce. [Kežmarok] : Jadro, 2013. [265] s. ISBN 978-8089426-26-3.
KLINGOVÁ, Adriana - KLING, Peter (zost.). Technické pamiatky spojené s banskou a hutníckou činnosťou na Spiši : III. časť - severozápadná časť Spiša. [Spišská Nová Ves] : Rochus - rozvoj Spiša, 2014. 229 s. ISBN 978-80-971834-2-4.
LACKO, Miroslav. Slovenská montánna historiografia v rokoch 1983 - 2005. Bratislava : Vlastný náklad autora, 2007. 84 s. ISBN 978-80-969780-4-5.
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