辽东五龙金矿床构造控矿特征和辉钼矿Re-Os年龄

肖昌浩; 刘向冲; 赵岩; 张青; 陈正乐; 刘建民; 韦昌山; 姚晓峰; 王伟; 解丽强

doi:10.3799/dqkx.2020.217

Volume 45 Issue 11

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(11): 3982-3997

Xiao Changhao, Liu Xiangchong, Zhao Yan, Zhang Qing, Chen Zhengle, Liu Jianmin, Wei Changshan, Yao Xiaofeng, Wang Wei, Xie Liqiang, 2020. Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China. Earth Science, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217

Citation:

Xiao Changhao, Liu Xiangchong, Zhao Yan, Zhang Qing, Chen Zhengle, Liu Jianmin, Wei Changshan, Yao Xiaofeng, Wang Wei, Xie Liqiang, 2020. Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China. Earth Science, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217

Citation:

Xiao Changhao, Liu Xiangchong, Zhao Yan, Zhang Qing, Chen Zhengle, Liu Jianmin, Wei Changshan, Yao Xiaofeng, Wang Wei, Xie Liqiang, 2020. Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China. Earth Science, 45(11): 3982-3997. doi: 10.3799/dqkx.2020.217

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Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China

doi: 10.3799/dqkx.2020.217

Xiao Changhao^{1, 2
,
,},
Liu Xiangchong^{1, 2},
Zhao Yan³,
Zhang Qing^{1, 2},
Chen Zhengle^{1, 2},
Liu Jianmin^{1, 2},
Wei Changshan^{1, 2},
Yao Xiaofeng⁴,
Wang Wei⁵,
Xie Liqiang⁶

1.
Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China
3.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
4.
Development and Research Center, China Geological Survey, Beijing 100037, China
5.
103 Branch of Non-Ferrous Geological Bureau of Liaoning Province, Dandong 118008, China
6.
Liaoning Wulong Gold Mining Corporation Limited, Dandong 118008, China

Received Date: 2020-07-23
Publish Date: 2020-11-15

Abstract

Abstract

The Wulong gold deposit is one of the most representative quartz-vein gold deposits in the Liaodong district in the NE China. The ore bodies and dikes are controlled by faults. The geometry,kinematics and kinetics characteristics of the ore-bearing structures indicate that the structural framework in the Wulong gold district is composed of the N-S tensile fracture,several NE-striking sinistral and NW-striking dextral conjugate faults and associated conjugate riedal fractures caused by the nearly N-S compression at the beginning of the Early Cretaceous. The diorites,Sanguliu pluton and Wulongbei pluton intruded into the pre-existing structures and NE-striking normal faults accompanied with the NW-SE extension during the Early Cretaceous. Hydrothermal fluid exsolution from the Early Cretaceous magmas migrated into the residual space in the fractures which were intruded by diorite. The dextral shear deformation led to the break of the quartz. The fractures infilled by granite dikes and quartz vines reactivated and the ore-forming fluids were characterized by vertical transport and lateral replacement in these fractures. The fluids infilled into the fractures of the broken quartz and replaced the Early Cretaceous dikes and gneissic monzonite granite. Therefore,the auriferous quartz veins share the similar space with the previous quartz and dikes. Kinetic characteristics of the ore-bearing structures indicate that the north of the NE-striking faults has the exploration potential and has a similar regularity for lateral trending of orebodies in the Sanshandao gold belt,Jiaodong district. In the Wulong gold district,the exploration potential of NE-striking faults is better than in the NW-striking faults and the tensile fractures in the footwall blocks of NE-striking faults are the advantageous space for searching for the concealed orebodies. This study first defines a molybdenite Re-Os isotopic model age of 125 ±2.1 Ma for the molybdenite-pyrite-pyrrhotite-quartz stage which represents the major ore-forming stage of the Wulong gold deposit. The Re concentrations of the molybdenite is 12.8×10^-6,suggesting that ore-forming material contained a mixture of crustal and mantle components. The comparison of previous studies indicate that both of the molybdenum and gold mineralization are related with the intense crust-mantle magma activity in NE China. In comparison with the metallogenic series in the Jiaodong district,both of the Liaodong and Jiaodong have two stages of molybdenum mineralization. Especially,the late of the Early Cretaceous molybdenum mineralization could be one of the clues for gold prespecting in the Liaodong district.
- structural control,
- molybdenite Re-Os dating,
- Wulong gold deposit,
- Liaodong,
- Jiaodong,
- geochronology

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Structural Controls and Re-Os Dating of Molybdenite of Wulong Gold Deposit, NE China

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