交代岩石圈地幔与金成矿作用

汪在聪; 王焰; 汪翔; 程怀; 许喆

doi:10.3799/dqkx.2021.221

Volume 46 Issue 12

Dec. 2021

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Article Navigation > Earth Science > 2021 > 46(12): 4197-4229

Wang Zaicong, Wang Christina Yan, Wang Xiang, Cheng Huai, Xu Zhe, 2021. Metasomatized Lithospheric Mantle and Gold Mineralization. Earth Science, 46(12): 4197-4229. doi: 10.3799/dqkx.2021.221

Citation:

Wang Zaicong, Wang Christina Yan, Wang Xiang, Cheng Huai, Xu Zhe, 2021. Metasomatized Lithospheric Mantle and Gold Mineralization. Earth Science, 46(12): 4197-4229. doi: 10.3799/dqkx.2021.221

Wang Zaicong, Wang Christina Yan, Wang Xiang, Cheng Huai, Xu Zhe, 2021. Metasomatized Lithospheric Mantle and Gold Mineralization. Earth Science, 46(12): 4197-4229. doi: 10.3799/dqkx.2021.221

Citation:

Wang Zaicong, Wang Christina Yan, Wang Xiang, Cheng Huai, Xu Zhe, 2021. Metasomatized Lithospheric Mantle and Gold Mineralization. Earth Science, 46(12): 4197-4229. doi: 10.3799/dqkx.2021.221

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Metasomatized Lithospheric Mantle and Gold Mineralization

doi: 10.3799/dqkx.2021.221

1.
State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
CAS Key Laboratory of Mineralogy and Metallogeny, Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
3.
Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou 510075, China

Received Date: 2021-10-07
Publish Date: 2021-12-15

Abstract

Abstract

Metasomatized lithospheric mantle has been considered to play a key control on the formation of giant gold (Au) deposits. Investigating the extent of Au enrichment in the metasomatized lithospheric mantle source and Au contents of mantle-derived magmas, as well as the mechanisms that promote the transportation and enrichment of Au from mantle source to large Au mineralization, could help us to understand the major controls responsible for the formation of giant hydrothermal Au deposits. Gold is one of the highly chalcophile elements and is also mobile in fluids. The behavior of Au in many processes such as mantle melting/metasomatism, magmatic-hydrothermal evolution, and mineralization is complicated. In this study, it compiles Au contents of mantle rocks and their derivative mafic magmas, and attempts to clarify key factors that control the behavior of Au from mantle, magmatic-hydrothermal processes to gold mineralization. It suggests that the metasomatized lithospheric mantle is an important source for giant hydrothermal Au deposits, but the remarkable Au enrichment of such mantle source is not necessarily required. Metasomatic components, especially volatiles, enable efficient release of Au from the mantle source to hydrous magmas and promote subsequent transportation and enrichment during magmatic-hydrothermal processes through trans-lithospheric fault systems. It thus emphasizes the main role of the metasomatized lithospheric mantle as the source of giant Au deposits and highlight the importance of metasomatic volatiles and related magmatic-hydrothermal processes in Au enrichment rather than anomalously pre-enriched sources or primary magmas. Therefore, understanding the behavior of Au in mantle metasomatism and magmatic-hydrothermal processes during the long-term evolution of the lithospheric mantle is the key to decode the genesis of giant hydrothermal Au deposits.
- lithospheric mantle,
- metasomatism,
- gold mineralization,
- chalcophile element,
- volatile,
- geochemistry

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References(255)

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Metasomatized Lithospheric Mantle and Gold Mineralization

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