Pyrite mineralization in upper precambrian black shales in the rybachi peninsula

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
Schlagworte:
Diagenesis
Geochemistry
Hydrogen sulfide
Hydrogen sulphide
Mineralization
Mineralogy
Oil shale
Petrology
Precambrian
Pyrite
Sedimentary facies
Shales
Sulphides
Turbidites
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creator Negrutsa, V Z
Polekhovskii, Yu S
Petrovskii, M N
Tarasova, I P
description 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.
doi_str_mv 10.1007/BF02782675
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1573-8892
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subjects Diagenesis
Geochemistry
Hydrogen sulfide
Hydrogen sulphide
Mineralization
Mineralogy
Oil shale
Petrology
Precambrian
Pyrite
Sedimentary facies
Shales
Sulphides
Turbidites
title Pyrite mineralization in upper precambrian black shales in the rybachi peninsula
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