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Wang B.,Shijiazhuang University of Economics | Niu S.,Shijiazhuang University of Economics | Sun A.,Shijiazhuang University of Economics | Liu Y.,Shijiazhuang University of Economics | And 5 more authors.
Chinese Journal of Geochemistry | Year: 2010

This study was conducted following research on metallogenesis in the Zhangjiajie-Xuanhua and East Hebei mantle branch structure zones. The Fuping mantle branch structure zone is one where Au, Cu and Ag polymetallic ore resources are concentrated in North Hebei. However, there has existed a long-standing controversy on the temporal-spatial distribution of ore resources and their ore-forming material sources. In terms of age dating and the comprehensive analysis of S, Pb, O, C and Si isotopes, it is considered that the temporal-spatial distribution of ore resources in this mantle branch structure zone is obviously controlled by the Fuping mantle branch structure. In space there is developed such a metallogenic pattern as to be Ag, Pb and Zn polymetallic ore deposits with gold appearing inside and copper appearing outside. Metallogenesis is dated mainly at Yanshanian, the ore-forming materials were derived predominantly from the deep interior of the Earth, and ore-forming fluids were derived largely from Yanshanian magmatism. © 2010 Science Press, Institute of Geochemistry, CAS and Springer Berlin Heidelberg. Source

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