中文摘要：

这研究被进行在 Zhangjiajie-Xuanhua 和东方 Hebei 披风分支结构地区在 metallogenesis 上跟随研究。Fuping 披风分支结构地区是 Au， Cu 和 Ag polymetallic 矿石资源在北方 Hebei 被集中的。然而，在那里存在矿石资源和他们的形成矿石的材料的时间空间的分发上的长期的争吵采购原料。以标明日期的年龄和 S， Pb， O， C 和 Si 同位素的全面分析，在这个披风分支结构地区的矿石资源的时间空间的分发被 Fuping 披风分支结构显然控制，这被考虑。在在那里的空间被开发如此的一个 metallogenic 模式至于 polymetallic 矿石与黄金扔的 Ag， Pb 和 Zn 正在出现里面和铜出现外面。Metallogenesis 主要在 Yanshanian 被标明日期，形成矿石的材料从地球的深内部主要被导出，并且形成矿石的液体主要从 Yanshanian magmatism 被导出。

英文摘要：

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 poly-metallic 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.