湖南大义山矿田白沙子岭锡矿床Rb-Sr同位素等时线年龄及其地质意义

张晓军; 罗华; 吴志华; 范先旺; 熊俊; 杨杰; 牟金燚

doi:10.3799/dqkx.2014.124

Volume 39 Issue 10

Oct. 2014

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Article Navigation > Earth Science > 2014 > 39(10): 1322-1332

Zhang Xiaojun, Luo Hua, Wu Zhihua, Fan Xianwang, Xiong Jun, Yang Jie, Mou Jinyi, 2014. Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province. Earth Science, 39(10): 1322-1332. doi: 10.3799/dqkx.2014.124

Citation:

Zhang Xiaojun, Luo Hua, Wu Zhihua, Fan Xianwang, Xiong Jun, Yang Jie, Mou Jinyi, 2014. Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province. Earth Science, 39(10): 1322-1332. doi: 10.3799/dqkx.2014.124

Citation:

Zhang Xiaojun, Luo Hua, Wu Zhihua, Fan Xianwang, Xiong Jun, Yang Jie, Mou Jinyi, 2014. Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province. Earth Science, 39(10): 1322-1332. doi: 10.3799/dqkx.2014.124

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Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province

doi: 10.3799/dqkx.2014.124

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Hubei Institute of Geological Survey, Wuhan 430034, China
3.
The 417 Geological Team of Hunan Bureau of Geology and Mineral Resources, Hengyang 421001, China

Received Date: 2014-03-31
Publish Date: 2014-10-01

Abstract

Abstract

Dayishan ore field located in the north rim of the middle section of the Nanling metallogenic belt in South China fold zone, and at the intersection of Yangmingshan-Dayishan-Shangpu EW basement fault, Youxian-Ningyuan NE basement fault and Chenzhou-Shaoyang NW concealed deep fault, has been controlled by the Dayishan intrusive rock. The greisens-vein type tin deposit is one of the typical mineralization types in this ore field. The Rb-Sr geochronology of fluid inclusions in quartz of the ore veins is presented and its geological significance of the Baishaziling greisens-vein type tin deposit is discussed in this paper. The Rb-Sr isotopic dating of fluid inclusions of quartz is 160±1 Ma, which indicates that the tin deposit was likely formed in the peaks (160-150 Ma) of Mesozoic mineralization period of Nanling region, and the mineralization was closely related to the magmatic intrusion of the Middle Jurassic monzogranite of Dayishan intrusive rock, as a result of the post-magmatic hydrothermal mineralization. The initial ⁸⁷Sr/⁸⁶Sr value of the fluid inclusions is 0.706 79±0.003 66, which may indicate a mantle-derived fluid contribution to the ore-forming fluids.
- Rb-Sr,
- isotopes,
- quartz fluid inclusion,
- monzogranite,
- geochronology,
- mineral deposit

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References(75)

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Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province

doi: 10.3799/dqkx.2014.124

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