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- W2382813912 abstract "Based on the studies of sulfur and lead isotopes from the ores in the Nanjiaohe silver multi-metal deposit in Yunnan, the range of δ~(34)S value from ores is -2.18‰ to 5.95‰, with the average 2.15‰, closing to that of the basic rocks sulfur. This indicates the sulfur from the ores came from deep materials. In the plot of δ~(34)S(Sp-Ga) to δ~(34)S(Sp) and δ~(34)S(Ga)(D.M.Pinckney and T.A.Rafter, 1972), the total sulfur isotopic components of hydrothermal fluid can be identified to be -0.86‰～+4.42‰, with the average 1.78‰. This reveals that the source of ore sulfur is related to the Lincang granite and resulted from the (homogenization) of deep magma. The ore lead compositions are mainly located around the orogenic belt in the pattern of tectonic by Zartman and Doe. This demonstrates that the ore lead came from the mixed lead. Contrasting with the lead compositions of the Lincang granite, the ore lead is composed of the (Lincang) granite body mixed with metamorphic rocks of Lancang Group." @default.
- W2382813912 created "2016-06-24" @default.
- W2382813912 creator A5074740742 @default.
- W2382813912 date "2003-01-01" @default.
- W2382813912 modified "2023-09-24" @default.
- W2382813912 title "CHARACTERISTICS OF THE SULFUR AND LEAD ISOTOPES IN THE NANJIAOHE SILVER MULTI-METAL DEPOSIT, YUNNAN" @default.
- W2382813912 hasPublicationYear "2003" @default.
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