GMRAP ID | 3100 |
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Alternate names | Banksa Štiavnica, Na Sobove |
Tract name | Northern Carpathians (150pCu6004) |
Group name | Štiavnica Group |
Included sites | Group includes Banska tiavnica, Sementlov, and Vysoká-Zlatno deposits. |
Site status | deposit |
Country | Slovakia |
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State or province | Banskobystricky kraj |
Geographic location | 18.898652, 48.470635 |
Geologic map unit | 18.898652, 48.470635 |
Nearby data |
Deposit type | Porphyry copper |
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Deposit subtype | Cu-Au |
Age determination method | Geologic inference |
Age range | Miocene(?) |
Age reference | geologic inference |
Minerals | barite, chalcopyrite, electrum, epidote, galena, rhodonite, scheelite, sphalerite, tourmaline |
Associated rocks | granodiorite-, quartz diorite- quartz porphyry dikes |
Tectonic setting | postconvergence |
Stratigraphic age | Miocene(?) |
Development status | Past Producer |
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Major commodities | Cu, Au |
Minor commodities | Ag, Bi, Te |
Tonnage (Mt) | 80Mt |
Cu grade (%) | 0.5% |
Au grade (g/t) | 0.5g/t |
Ag grade (g/t) | 25g/t |
Contained copper | 400,000t |
Gold-Moly ratio | -9999 |
Comments | Abandoned, past production: 80 Mt at 25 g/t Ag; 80 Mt at 0.5 g/t Au; 2.7 Mt at 0.3% Cu; 3.7 Mt at 1.5% Pb; and 3.5 Mt at 2% Zn. The largest andesitic volcano in the Central Slovakian Neogene Volcanic Field, Banská tiavnica, has been a focus of mining of precious and base metals for a long time (Jelen and others, 2003). In the greater Banská tiavnica intrusive complex, several types of mineral deposits have been recognized, including the Banská tiavnica porphyry Cu-Mo-Au deposit and related occurrences. The porphyry deposit occurs in granodiorite-quartz-diorite porphyry dike clusters and in the rocks surrounding the granodiorite pluton (Jelen and others, 2003). West Carpathians. |
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Study area name | Europe |
References | Jele? and others (2003); Lips and others (2006) |
Site reference | Sutphin and others (2013) |