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REN Peng, LIANG Ting, LIU Kuo-long, et al. Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains[J]. Northwestern Geology, 2014, 47(1): 137-149.
Citation: REN Peng, LIANG Ting, LIU Kuo-long, et al. Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains[J]. Northwestern Geology, 2014, 47(1): 137-149.

Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains

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  • Received Date: January 04, 2014
  • Revised Date: February 22, 2014
  • Available Online: July 28, 2022
  • Published Date: March 04, 2014
  • Fengtai mineral cluster region is located in the middle of Qinling Devonian lead and zinc polymetallic metallogenic belt. Lead-zinc deposits are mainly located in the siliceous rocks between Gudaoling group of the Upper Devonian and Xinghongpu group of the Middle Devonian. The analysis of S and Pb isotopic compositions of ore minerals in three typical ore deposits indicates that δ34S values of metal sulfide range no more than 10‰ in Qiandongshan, Bafangshan and Yinmusi lead-zinc deposits. The δ34S values of sulfides in the region range from 4.3‰ to 13.2‰, indicating that sulfur mainly came from seawater sulfate reduction. Among the lead isotope of three deposits, 206Pb/204Pb varies from 17.775 to 18.180, 207Pb/204Pb varies from 15.457 to 15.805, and 208Pb/204Pb varies from 37.977 to 38.670. Pb isotopic compositions have a large overlap, suggesting that the three lead-zinc deposits have similar sources of lead. The analysis of structure model diagram and Δβγ diagram of Pb isotope shows that lead came from the process that Yangtze plate subducted to North China plate in the middle of Early Paleozoic and Qinling microplate subducted to North China plate in the late Paleozoic.
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