郯庐断裂带晚白垩世金成矿作用: 来自龙泉站金矿床黄铁矿Rb-Sr年代学证据

石文杰; 魏俊浩; 谭俊; 李艳军; 付乐兵; 李欢; 赵少卿; 田宁

doi:10.3799/dqkx.2014.031

Volume 39 Issue 3

Mar. 2014

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Article Navigation > Earth Science > 2014 > 39(3): 325-340

Shi Wenjie, Wei Junhao, Tan Jun, Li Yanjun, Fu Lebing, Li Huan, Zhao Shaoqing, Tian Ning, 2014. Late Early Cretaceous Gold Mineralization in Tan-Lu Fault Zone: Evidence from Rb-Sr Isotopic Dating of Pyrite from Longquanzhan Gold Deposit. Earth Science, 39(3): 325-340. doi: 10.3799/dqkx.2014.031

Citation:

Shi Wenjie, Wei Junhao, Tan Jun, Li Yanjun, Fu Lebing, Li Huan, Zhao Shaoqing, Tian Ning, 2014. Late Early Cretaceous Gold Mineralization in Tan-Lu Fault Zone: Evidence from Rb-Sr Isotopic Dating of Pyrite from Longquanzhan Gold Deposit. Earth Science, 39(3): 325-340. doi: 10.3799/dqkx.2014.031

Citation:

Shi Wenjie, Wei Junhao, Tan Jun, Li Yanjun, Fu Lebing, Li Huan, Zhao Shaoqing, Tian Ning, 2014. Late Early Cretaceous Gold Mineralization in Tan-Lu Fault Zone: Evidence from Rb-Sr Isotopic Dating of Pyrite from Longquanzhan Gold Deposit. Earth Science, 39(3): 325-340. doi: 10.3799/dqkx.2014.031

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Late Early Cretaceous Gold Mineralization in Tan-Lu Fault Zone: Evidence from Rb-Sr Isotopic Dating of Pyrite from Longquanzhan Gold Deposit

doi: 10.3799/dqkx.2014.031

Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2013-07-12
Publish Date: 2014-03-15

Abstract

Abstract

Longquanzhan gold deposit, an important part of gold mineralization belt of Yi-Shu fault zone, is the only altered tectonite-type gold deposit discovered in the area at present. The ore bodies mainly occur at the fracture zone and the footwall metamorphic rocks. Rb-Sr isotopic dating of 10 pyrites separated from the Longquanzhan gold deposit yields an isochron age of 96±2 Ma (MSWD=1.2), which is in good agreement with the late Early Cretaceous to early Late Cretaceous magmatism (106-96 Ma) in adjacent area of Yi-Shu fault zone. Meanwhile, combining with the precise ages of gold deposits in Shandong Province and mineral exploration data, we suggest that late Early Cretaceous gold mineralization may occur in the southeastern margin of North China Craton, and its tectonic setting is related to an extensional setting which resulted in a large-scale asthenosphere upwelling, accompanying decompression and isotherm upwelling, material exchange and mixing between mantle and crust, and finally providing a great amount of ore-forming fluids and materials for gold mineralization. According to the precise age of Longquanzhan gold deposit reported, this discovery is of great significance both in gold deposit origin contrast of both sides and future mineral exploration.
- Rb-Sr isotopic dating,
- Yi-Shu fault zone,
- ore-forming time,
- North China Craton,
- ore deposits,
- geochronology,
- Jiaodong,
- Luxi

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References(131)

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Late Early Cretaceous Gold Mineralization in Tan-Lu Fault Zone: Evidence from Rb-Sr Isotopic Dating of Pyrite from Longquanzhan Gold Deposit

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