Influences of ore formation on biomarkers in the Kupferschiefer from the Lubin mine, Poland

Molecular biomarkers are the important maturity parameters for sedimentary organic matter.They have also been widely used for determining the maturity of organic matter in ore deposits. However,during the study of organic matter in the Kupferschiefer from the Lubin mine, it had been found that the b...

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Published inActa geochimica Vol. 24; no. 2; pp. 101 - 107
Main Author 孙玉壮 陈建平 林明月 孟志强 张洪建
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Nature B.V 01.04.2005
Open Laboratory of Organic Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China%Key Laboratory for Petroleum Geochemistry, CNPC, Beijing 100083, China%Hebei University of Engineering, Handan 056038, China%China University of Mining and Technology, Xuzhou 221008, China
Hebei University of Engineering, Handan 056038, China
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ISSN1000-9426
2096-0956
1993-0364
2365-7499
DOI10.1007/BF02841152

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Summary:Molecular biomarkers are the important maturity parameters for sedimentary organic matter.They have also been widely used for determining the maturity of organic matter in ore deposits. However,during the study of organic matter in the Kupferschiefer from the Lubin mine, it had been found that the biomarkers were influenced by sulfide formation. In order to probe into the degree of influence on biomarkers, seven samples collected from a Kupferschiefer section from the Lubin mine were analyzed by various geochemical methods. The results indicated that in the samples with higher copper contents, the values of biomarkers are lower than in the samples with lower copper contents. In highly mineralized samples, hydrogen donation for thermochemical sulfate reduction (TSR) occurred in alkylated phenanthrenes and naphthalenes, leading to the decrease of 12 biomarker parameters during the Kupferschiefer mineralization.
Bibliography:P611.22
52-1043/P
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ISSN:1000-9426
2096-0956
1993-0364
2365-7499
DOI:10.1007/BF02841152