Szczegóły publikacji
Opis bibliograficzny
Teaching an old dog new tricks: local occurrences of massive Cu-Ag ($\pm$Ge, Re) mineralization in the Kupferschiefer deposit, Poland / Krzysztof FOLTYN, Władysław ZYGO, Mateusz Fendrych, Piotr Ducki, Jakub Węgrzynowicz // W: 16th IAGOD quadrennial symposium [Dokument elektroniczny] : the role of geoscience in the energy transition : August 31–September 2, 2026, [Porto, Portugal] : abstract book. — Wersja do Windows. — Dane tekstowe. — [Porto : University of Porto], [2026]. — S. 212–213. — Wymagania systemowe: Adobe Reader. — Tryb dostępu: https://iagod2026.inporto.events/docs/IAGOD_2026%20Abstract_V... [2026-09-22]. — Bibliogr. s. 213, Summ.
Autorzy (5)
- AGHFoltyn Krzysztof
- AGHZygo Władysław
- Fendrych Mateusz
- Ducki Piotr
- Węgrzynowicz Jakub
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 170170 |
|---|---|
| Data dodania do BaDAP | 2026-10-27 |
| Rok publikacji | 2026 |
| Typ publikacji | materiały konferencyjne (aut.) |
| Otwarty dostęp |  |
Abstract
The Cu–Ag mineralization of the Kupferschiefer in central Europe is generally regarded as being predominantly controlled by redox (reduction–oxidation) processes but here we report two examples of localized massive mineralization from Polish Kupferschiefer, where different mechanisms played a key role. The unique mineralization encountered in the GG1 shaft (Rudna mine) consists of massive covellite and galena, accompanied by acanthite, jalpaite (Ag3CuS2) and argyrodite (Ag8GeS6) and was found at the contact between Zechstein Limestone (Ca1) and Lower Anhydrite (A1d), approximately 5 m above the main copper orebody. In the Lubin mine, near the southern margin of the deposit, horizontal sulphide veins and lenses composed of massive chalcocite/djurleite, bornite, chalcopyrite, sphalerite, galena and covellite are developed locally. These bodies are hosted by altered, porous, organogenic carbonates in the areas where shale is absent, and exhibit features resembling carbonate-replacement type deposits. The massive chalcocite/djurleite and bornite are notably enriched in silver and contain <0.1-5.7 ppm of rhenium.
