湘西北五伦铅锌矿床闪锌矿Rb-Sr定年及其地质意义

曾广乾; 李泽泓; 凌跃新; 熊延旺; 马筱

doi:10.3799/dqkx.2018.566

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2484-2495

Zeng Guangqian, Li Zehong, Ling Yuexin, Xiong Yanwang, Ma Xiao, 2018. Rb-Sr Dating of Sphalerites from Wulun Lead-Zinc Deposit in Northwestern Hunan and Its Geological Significance. Earth Science, 43(7): 2484-2495. doi: 10.3799/dqkx.2018.566

Citation:

Zeng Guangqian, Li Zehong, Ling Yuexin, Xiong Yanwang, Ma Xiao, 2018. Rb-Sr Dating of Sphalerites from Wulun Lead-Zinc Deposit in Northwestern Hunan and Its Geological Significance. Earth Science, 43(7): 2484-2495. doi: 10.3799/dqkx.2018.566

Citation:

Zeng Guangqian, Li Zehong, Ling Yuexin, Xiong Yanwang, Ma Xiao, 2018. Rb-Sr Dating of Sphalerites from Wulun Lead-Zinc Deposit in Northwestern Hunan and Its Geological Significance. Earth Science, 43(7): 2484-2495. doi: 10.3799/dqkx.2018.566

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Rb-Sr Dating of Sphalerites from Wulun Lead-Zinc Deposit in Northwestern Hunan and Its Geological Significance

doi: 10.3799/dqkx.2018.566

1.
Hunan Institute of Geological Survey, Changsha 410016, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2017-11-29
Publish Date: 2018-07-15

Abstract

Abstract

The Wulun lead-zinc deposit lies to the northwest of Jiangnan (Xuefeng) orogenic belt on the southeastern margin of Yangtze block, as a newly discovered hydrothermal vein type of lead-zinc deposit in the lead-zinc ore belt along the Wanmingang anticline in northwestern Hunan. The ore bodies outcrop in the Lower Ordovician Tongzi and Honghuayuan formations as steep-dipping veins controlled by NW trending faults which derived by NE trending Bitiexi-Chenjiahe fault. Rb-Sr dating of sphalerite yielded an isochron age of 238.9±4.5 Ma (MSWD=1.8) with initial ⁸⁷Sr/⁸⁶Sr value of 0.710 86±0.000 16 for the deposit, which shows that the end of Middle Triassic is the main mineralization period for the Wulun lead-zinc deposit. Integrated with the existing metallogenic geochronology data, and the discussing of the geodynamical setting, it is indicated that there are at least twice lead-zinc mineralization in northwestern Hunan, which was respectively related to the post-orogenic extension of late Caledonian tectonism and the local stretching derived from collision of South China block in the early Indosinian. The metallogenic materials of Wulun lead-zinc deposit shall be mainly derived from the clastic rocks with high ore-forming elements in the Nanhua-Early Cambrian stratas underlying the ore-bearing layers. The relatively high initial Sr isotope ratio indicates that the influence of continental crust was obvious in the metallogenic process.
- sphalerite Rb-Sr dating,
- mineralization age,
- material source,
- Wulun lead-zinc deposit,
- northwestern Hunan Province,
- isotopes

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References(93)

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