Structural Systems of Fankou Lead-Zinc Orefield in Renhua County, Guangdong Province, China

Ying Shu Li; Dong Ming Yang; Da Qing He; Jiao Jiao Chen; Yi Ke Zhang; Cheng Lin Yang; Yan Cai

doi:10.4028/www.scientific.net/AMR.807-809.2267

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 807-809Structural Systems of Fankou Lead-Zinc Orefield in...

Structural Systems of Fankou Lead-Zinc Orefield in Renhua County, Guangdong Province, China

Abstract:

Orefield structures of Fankou lead-zinc deposit in Guangdong province is complex and have been argued about for years. On the basis of the theory and method of the geomechanics, the mechanics features of structural planes of the structures of Fankou lead-zinc orefield have been identified. Its indicated that its structure is divided into three types of systems, that is, the northwest trending structural belt which origin from the Caledonian stage to the Hercynian stage, the Lambda-type structure which origin from the Indo-Chinese stage to the Yanshan stage and the eastweat trending structural belt which origin the Himalayan stage. The lambda-type structure made of major fault of F₂₀₃ of strike northwest and branch fault of F₃, F₄ of strike northnortheast is identified as the structural system of mineralization.

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Periodical:

Advanced Materials Research (Volumes 807-809)

Pages:

2267-2271

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.807-809.2267

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Online since:

September 2013

Authors:

Ying Shu Li*, Dong Ming Yang, Da Qing He, Jiao Jiao Chen, Yi Ke Zhang, Cheng Lin Yang, Yan Cai

Keywords:

Fankou in Guangdong Province, China, Pb-Zn Ore Deposit, Structure System

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* - Corresponding Author

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