首页> 外文期刊>Chinese Journal of Geochemistry >Geochemical characteristics of the Jinjiazhuang ultrabasic Roch-Type Gold Deposit in chicheng County, Hebei Province
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Geochemical characteristics of the Jinjiazhuang ultrabasic Roch-Type Gold Deposit in chicheng County, Hebei Province

机译:河北省赤城县金家庄超碱性罗奇型金矿床地球化学特征

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摘要

The Jinjiazhuang gold deposit occurs in the zhangjiakou gold field, Northwest Hebei. The ore bodies are mostly hosted in Xiaozhangjiakou ultraasic rocks dominated by Diopsidite. Electron microprobe analyses indicate that the deposit is characterized by the enrich- Ment of some platinum group elements in principal metallic minerals such as chalcopyrite, gale- Na, sphalerite and pyrite, and the presence of millerite. Stable isotope studies show that car- Bon, sulfur and most of the metallogenic elements were probably derived largely from the host Xiaozhangjiakou ultrabasic rocks and that it is possible that the ore-forming fluid was predomi- Nated by meteoric water.
机译:金家庄金矿床位于河北西北部张家口金矿区。矿体主要存在于以蛇纹石为主的小张家口成岩岩中。电子探针分析表明,该矿床的特征是主要金属矿物(如黄铜矿,加勒钠,闪锌矿和黄铁矿)中某些铂族元素的富集以及存在辉石。稳定的同位素研究表明,车邦,硫和大部分成矿元素可能主要来自于小张家口超基性岩体,并且成矿流体可能被陨石水所占优势。

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