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- W2350135039 abstract "There are a lot of organic matters in different forms or maturity in the Jinding zinc-lead deposit and Lanping basin. The content of organic matter increases obviously from Lanping basin to Jinding deposit and the organic matters in the ores and wall-rocks in the Jinding deposit are in mature and high-mature stages. The geochemical characteristics of the organic matters in the deposit show that the organic matters of the source rocks were mainly derived from bacteria and algae, and are type-Ⅰorganic matter. The source rocks experienced high reduction evolution and in the high salinity environments. The Pb isotopic compositions indicated that the bitumen in the ore district was derived from the organic matters in the Lanping basin. The C isotopic compositions showed that the organic matters were closely related to metal mineralization. During the process of basin evolution, hydrocarbon reservoir formed in the Jinding dome is the reducer of rapid metal mineralization." @default.
- W2350135039 created "2016-06-24" @default.
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- W2350135039 date "2008-01-01" @default.
- W2350135039 modified "2023-10-03" @default.
- W2350135039 title "Geochemistry of organic matters in the Jinding zinc-lead deposit, Lanping Basin, Northwest Yunnan Province" @default.
- W2350135039 hasPublicationYear "2008" @default.
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