辽东三股流岩体是否为五龙金矿成矿提供必要的能量？

刘向冲; 肖昌浩; 张拴宏; 胡国辉; 李建锋; 王晨光

doi:10.3799/dqkx.2020.292

Volume 45 Issue 11

Nov. 2020

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Article Navigation > Earth Science > 2020 > 45(11): 3998-4013

Liu Xiangchong, Xiao Changhao, Zhang Shuanhong, Hu Guohui, Li Jianfeng, Wang Chenguang, 2020. Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?. Earth Science, 45(11): 3998-4013. doi: 10.3799/dqkx.2020.292

Citation:

Liu Xiangchong, Xiao Changhao, Zhang Shuanhong, Hu Guohui, Li Jianfeng, Wang Chenguang, 2020. Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?. Earth Science, 45(11): 3998-4013. doi: 10.3799/dqkx.2020.292

Citation:

Liu Xiangchong, Xiao Changhao, Zhang Shuanhong, Hu Guohui, Li Jianfeng, Wang Chenguang, 2020. Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?. Earth Science, 45(11): 3998-4013. doi: 10.3799/dqkx.2020.292

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Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?

doi: 10.3799/dqkx.2020.292

Liu Xiangchong^{1, 2, 3
,
,},
Xiao Changhao^{1, 2, 3},
Zhang Shuanhong^{1, 3},
Hu Guohui^{1, 3},
Li Jianfeng^{1, 3},
Wang Chenguang⁴

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, CAGS, Beijing 100081, China
3.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China
4.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2020-05-18
Publish Date: 2020-11-15

Abstract

Abstract

The Wulong gold deposit located in Liaoning Province is a typical vein-type gold deposit in the eastern part of the North China craton,but how this large-scale gold deposit formed remains controversial. This deposit was interpreted to be genetically related to the Sanguliu granite because they are spatially close and have close chronological ages and the mineralizing fluids have a magmatic-hydrothermal origin. There is no sufficient evidence supporting that the Sanguliu granite provided the gold-bearing magmatic-hydrothermal fluids required for forming the Wulong deposit,so did the former provide sufficient energy for the latter? In order to answer this question,numerical modeling of heat-driven convection of meteoric water and magmatic-hydrothermal fluids released by the Sanguliu granite was built based on its geochemical and geophysical characteristics to simulate the evolution of fluid flow and temperature after emplacement of the granite. Numerical results indicate that the temperatures within 1 km of the Sanguliu granite were elevated to over 300℃ for hundreds of thousands of years. This long high temperature filed favors formation of magmatic-hydrothermal deposits. In contrast,the position of the Wulong deposit received insignificant energy from the Sanguliu granite. If magmatic-hydrothermal fluids were released from the Sanguliu granite,those magmatic-hydrothermal fluids should have caused alteration and minerlization at the granite margin and the contact between the granite and its wallrock. However,these phenomena have not been identified in the field. Therefore,there is probably no genetic relationship between the large-scale Wulong deposit and the Sanguliu granite,and further investigations are needed to identify the source for Au-mineralizing fluids.
- Sanguliu granite,
- Wulong gold deposit,
- fluid convection,
- numerical simulation,
- magmatic-hydrothermal fluid,
- mineral deposits

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References(95)

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Whether Sanguliu Granite Provided Energy Required for Forming Wulong Gold Deposit, Liaoning Province, China?

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