Pyrite mineralization in upper precambrian black shales in the rybachi peninsula

Spatiotemporal regularities of the sulfide mineralization distribution in shales of the Skorbeev Formation, as well as the results of its study, have been analyzed. Their genetic relation to distal facies of the fan turbidite system has been substantiated. Ore minerals are predominantly represented...

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Veröffentlicht in:Lithology and Mineral Resources 2000-03, Vol.35 (2), p.131-140
Hauptverfasser: Negrutsa, V Z, Polekhovskii, Yu S, Petrovskii, M N, Tarasova, I P
Format: Artikel
Sprache:eng
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Zusammenfassung:Spatiotemporal regularities of the sulfide mineralization distribution in shales of the Skorbeev Formation, as well as the results of its study, have been analyzed. Their genetic relation to distal facies of the fan turbidite system has been substantiated. Ore minerals are predominantly represented by pyrite formed at an early diagenesis stage in conditions of hydrogen sulfide-bacterial paleoecosystems and repeatedly altered in the process of subsequent sediment transformation.
ISSN:0024-4902
1608-3229
1573-8892
DOI:10.1007/BF02782675