Relationship between Yanshanian Granites and Multi-Metal Mineralization of Tungsten in South China

With the new discovery of the world's largest tungsten deposit (the Zhuxi tungsten-copper polymetallic deposit) in the Taqian-Fuchun mineralization concentration area, it has attracted great attention in the industry peers. On the basis of the previous research and latest exploring results, this paper makes a systematical summary and discussion on the regional ore-forming geological conditions, ore deposit types and mineralization regularity, tectonic-magmatic-mineralization. The results showed that this area has experienced multi-phase tectonic-magmatic activities since Jinningian, tungsten-copper polymetallic deposit closely related with Yanshanian tectonic-magmatic activities. The deposit types are mainly skarn type, porphyry (altered granite) type and vein (fracture zone) type. It presents belt distribution in northeast and cluster distribution in northwest. The regional northeast Nappe structure controls deposit distribution, while thrust nappe structure, unconformable contact structure, intrusive contact structure, tension structure, interlayer fracture and broken zone structure directly control the formation of deposit and spatial location of ore bodies.

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Features and Potential Analysis of the Lingxi Polymetallic Mineralization Area in the Periphery of Lengshuikeng Ore Field

明¹

2018

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Relationship between Yanshanian Granites and Multi-Metal Mineralization of Tungsten in South China

Cited by 3 publications

References 1 publication

Temporal and spatial relationships of granitic magmatism and W mineralization: Insights from the Xingguo orefield, South China

Temporal and spatial relationships of granitic magmatism and W mineralization: Insights from the Xingguo orefield, South China

Tectonization-Magmation-Mineralization of the Taqian-Fuchun W-Cu Polymetallic Mineralization Concentration Area

Features and Potential Analysis of the Lingxi Polymetallic Mineralization Area in the Periphery of Lengshuikeng Ore Field

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