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We describe detrital gold grains obtained from sediments from the Skora River bed in the North Sudetic Trough, focussing on identification of microinclusions of ore minerals, combined with analyses of grain morphology and their chemical composition, to constrain the origin of the detrital gold. A population of gold grains of natural origin was identified, represented mostly by phases of native gold. A few microinclusions of Pd selenides and tellurides were identified, suggesting that local outcrops of the Rotliegend-Zechstein boundary zone are the probable source areas for the gold grains. In addition, a large population of amalgams of probable anthropogenic origin was identified. Their identification is of potential importance in the study of environmental mercury contamination, while distinguishing between the two grain populations is crucial to studying the origin of modern placer gold deposits.
Słowa kluczowe
Czasopismo
Rocznik
Tom
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art. no. 35
Opis fizyczny
Bibliogr. 74 poz., rys., wykr.
Twórcy
autor
- “Poltegor-Institute” Opencast Mining Institute, Department of Geology, Parkowa 25, 51-616 Wrocław, Poland
autor
- University of Wrocław, Faculty of Earth Sciences and Environmental Management, Department of Mineral Resources Management, Plac Maxa Borna 9, 50-204 Wrocław, Poland
Bibliografia
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Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2025).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c9c23ffe-8fda-4b21-b25c-4c926ffa82f4
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