湘西花垣矿集区柔先山铅锌矿床的成矿时间和物质来源

谭娟娟; 刘重芃; 杨红梅; 蔡应雄; 卢山松

doi:10.3799/dqkx.2018.132

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2438-2448

Tan Juanjuan, Liu Chongpeng, Yang Hongmei, Cai Yingxiong, Lu Shansong, 2018. Geochronology and Ore-Forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area, Western Hunan. Earth Science, 43(7): 2438-2448. doi: 10.3799/dqkx.2018.132

Citation:

Tan Juanjuan, Liu Chongpeng, Yang Hongmei, Cai Yingxiong, Lu Shansong, 2018. Geochronology and Ore-Forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area, Western Hunan. Earth Science, 43(7): 2438-2448. doi: 10.3799/dqkx.2018.132

Citation:

Tan Juanjuan, Liu Chongpeng, Yang Hongmei, Cai Yingxiong, Lu Shansong, 2018. Geochronology and Ore-Forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area, Western Hunan. Earth Science, 43(7): 2438-2448. doi: 10.3799/dqkx.2018.132

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Geochronology and Ore-Forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area, Western Hunan

doi: 10.3799/dqkx.2018.132

Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2018-04-17
Publish Date: 2018-07-15

Abstract

Abstract

In Western Hunan-Eastern Guizhou metallogenetic belt, the Huayuan ore concentration area with ten-million-tons expected reserves of Pb and Zn, is one of the world-class super-large Pb-Zn ore deposits. Rouxianshan Pb-Zn deposit located in the center of Huayuan area, is a typical deposit in the Yutang ore field. This study carries out Rb-Sr geochronology study of sphalerites from Rouxianshan, and utilizes phase-seperation method to achieve an ideal Rb-Sr isochron line, yielding an Early Devonian age of 412±6 Ma (MSWD=1.5, initial ⁸⁶Sr/⁸⁷Sr=0.709 32), which is meaningful for constraining the ore-forming age in Huayuan area. The fluid inclusions, Sr-S-Pb isotopic composition of ore samples from Rouxianshan have also been analyzed. The results indicate that the ore-forming fluid may have originated from a mixture of strata-sealed water and transporting fluid, and the ore is characterized by Pb-Sr isotopic composition from upper crust. Further, the Pb in ores mainly comes from the wall rocks, and the S attributed to the thermo-chemical sulfate reduction (TSR) of overlying gypsum-bearing rock formation.
- Huayuan ore-concentration area,
- Rouxianshan ore,
- Pb-Zn deposit,
- sphalerite Rb-Sr isochron line,
- isotope,
- ore-forming fluid,
- geochemistry

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References(78)

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Geochronology and Ore-Forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area, Western Hunan

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