| Reference Type | Journal (article/letter/editorial) |
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| Title | Mineral Assemblages And Genesis Of The Cu-Au Epithermal Deposits In The Southern Part Of The Panaguyrishte Ore District, Bulgaria |
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| Journal | Bulletin of the Geological Society of Greece |
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| Authors | Bogdanov, K. | Author |
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| Tsonev, D. | Author |
| Popov, K. | Author |
| Bogdanov, K. | Author |
| Tsonev, D. | Author |
| Popov, K. | Author |
| Year | 2004 (January 1) | Volume | 36 |
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| Page(s) | 406-415 | Issue | 1 |
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| Publisher | National Documentation Centre (EKT) |
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| URL | |
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| DOI | doi:10.12681/bgsg.16726Search in ResearchGate |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 597148 | Long-form Identifier | mindat:1:5:597148:4 |
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| GUID | 0 |
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| Full Reference | Bogdanov, K., Tsonev, D., Popov, K. (2004) Mineral Assemblages And Genesis Of The Cu-Au Epithermal Deposits In The Southern Part Of The Panaguyrishte Ore District, Bulgaria. Bulletin of the Geological Society of Greece, 36 (1). 406-415 doi:10.12681/bgsg.16726 |
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| Plain Text | Bogdanov, K., Tsonev, D., Popov, K. (2004) Mineral Assemblages And Genesis Of The Cu-Au Epithermal Deposits In The Southern Part Of The Panaguyrishte Ore District, Bulgaria. Bulletin of the Geological Society of Greece, 36 (1). 406-415 doi:10.12681/bgsg.16726 |
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| In | (2004, January) Bulletin of the Geological Society of Greece Vol. 36 (1) National Documentation Centre (EKT) |
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| Abstract/Notes | Epithermal Cu-Au deposits hosted within volcanic rocks (Radka, Elshitsa, Krassen) are related to Late Cretaceous andesite-dacite volcanic terrain in the Panagyurishte ore district. The Cu-Au ores are linked by a similar mineralogy and differ by the ratio of tennantite, bornite, enargite and discrete trace minerals of Ga, Ge, In and Bi (e.g., roquesite, germanite, betekhtinite, renierite, vinciennite, aikinite). Bi-Se-Te and Ga-Ge-ln-Sn signature with pronounced Au-enrichment of the bornite rich ores is a characteristic feature underlying the increasing role of the fS2/f02 control during the transition from IS te HS environment. Formation of the epithermal Cu-Au deposits appears to have occurred during a single broad event of contemporaneous formation of epithermal and porphyry systems.The close connection between the volcano-plutonic structures facilitates the multistage and polycyclic character of their hydrothermal systems, the similar character of the epithermal ores and the mineral succession in Elshitsa, Radka and Krassen deposits. The ô^S ratios in the sulphide minerals range from -6.7 to 4.0, suggesting comparable magmatic sources for the epithermal mineralizing fluids and close link with porphyry environment. |
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| Locality | Mineral(s) |
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| Panagyurishte Municipality, Pazardzhik Province, Bulgaria | ⓘ Friedrichite, ⓘ Hammarite, ⓘ Heulandite Subgroup, ⓘ Laumontite, ⓘ Mordenite, ⓘ Stilbite Subgroup |
| Elshitsa mine, Elshitsa, Panagyurishte Municipality, Pazardzhik Province, Bulgaria | ⓘ Aikinite, ⓘ Albite, ⓘ Altaite, ⓘ Anhydrite, ⓘ Baryte, ⓘ Bornite, ⓘ Calcite, ⓘ Cassiterite, ⓘ Chalcopyrite, ⓘ Chlorite Group, ⓘ Covellite, ⓘ Diaspore, ⓘ Enargite, ⓘ Epidote, ⓘ Galena, ⓘ Gypsum, ⓘ Hessite, ⓘ Illite, ⓘ Magnetite, ⓘ Marcasite, ⓘ Muscovite, ⓘ Native Bismuth, ⓘ Native Gold, ⓘ Pyrite, ⓘ Quartz, ⓘ Rutile, ⓘ Sericite, ⓘ Smectite Group, ⓘ Sphalerite, ⓘ Tennantite Subgroup, ⓘ Tetradymite, ⓘ Tetrahedrite Subgroup, ⓘ Titanium-bearing Magnetite |
| Radka Mine, Levski, Panagyurishte Municipality, Pazardzhik Province, Bulgaria | ⓘ Aikinite, ⓘ Anhydrite, ⓘ Bismuthinite, ⓘ Bornite, ⓘ Briartite, ⓘ Buckhornite, ⓘ Chalcocite, ⓘ Chalcopyrite, ⓘ Covellite, ⓘ Electrum, ⓘ Enargite, ⓘ Galena, ⓘ Gallite, ⓘ Germanite, ⓘ Goldfieldite, ⓘ Gypsum, ⓘ Illite, ⓘ Kësterite, ⓘ Kiddcreekite, ⓘ Muscovite, ⓘ Native Gold, ⓘ Native Silver, ⓘ Pyrite, ⓘ Quartz, ⓘ Renierite, ⓘ Roquesite, ⓘ Sericite, ⓘ Smectite Group, ⓘ Sphalerite, ⓘ Stannite, ⓘ Tennantite Subgroup, ⓘ Tsumoite, ⓘ Vinciennite, ⓘ Wittichenite |
| Krassen Mine, Popintsi, Panagyurishte Municipality, Pazardzhik Province, Bulgaria | ⓘ Aikinite, ⓘ Bornite, ⓘ Chalcopyrite, ⓘ Covellite, ⓘ Dickite, ⓘ Enargite, ⓘ Illite, ⓘ Kaolinite, ⓘ Muscovite, ⓘ Native Gold, ⓘ Pyrite, ⓘ Quartz, ⓘ Sericite, ⓘ Smectite Group |
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