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Supergénne minerály stratiformnej U-Cu mineralizácie pri Spišskej Teplici (hronikum, Kozie chrbty, východné Slovensko)
Názov Supergénne minerály stratiformnej U-Cu mineralizácie pri Spišskej Teplici (hronikum, Kozie chrbty, východné Slovensko) Súbež.n. Supergene minerals of stratiform U-Cu mineralization at Spišská Teplica (Hronicum Unit, Kozie chrbty Mts., Eastern Slovakia) Aut.údaje Štefan Ferenc, Eva Hoppanová ... [et al.] Autor Ferenc Štefan 1977- (35%) UMBFP01 - Katedra geografie a geológie
Spoluautori 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
Zdroj.dok. Bulletin Mineralogie Petrologie. Vol. 28, no. 2 (2020), pp. 295-306. - Praha : Mgr. Jiří Sejkora, 2020 Kľúč.slová urán - uranium meď - copper malachite azurite Heslá geogr. Kozie chrbty Západné Karpaty (pohorie) Spiš (Slovensko : oblasť) Form.deskr. články - journal articles Jazyk dok. slovenčina Krajina Česká republika Anotácia 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 Kategória publikačnej činnosti ADM Číslo archívnej kópie 49309 Katal.org. BB301 - Univerzitná knižnica Univerzity Mateja Bela v Banskej Bystrici Báza dát xpca - PUBLIKAČNÁ ČINNOSŤ Odkazy PERIODIKÁ-Súborný záznam periodika 
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