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《Geochimica》 1998-02
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TRACE ELEMENT GEOCHEMICAL AND STABLE ISOTOPIC STUDY OF THE HULISHAN GOLD DEPOSITS IN YUANPING, SHANXI PROVINCE

Chang Xiangyang;Tian Yongqing (Guangzhou Institute of Geochemisiry, Chinese Academy of Sciences, Guangzhou 510640)(Shanxi Institute of Geological Sciences. Taiyuan 030006)  
The geological and trace element geochemical characteristics show that shear deformation zone should be the principal controlling factors of the gold mineralization at Hulishan gold deposits in western Wutaishan region, Shanxi Province. The REE patterns and S, H O, C, Ph stable isotope data indicate that metallogenetic materials come principally from greenstone strata, and ore-forming hydrothermal fluid is characterized by multiple sources. The gold mineralization took place (2230 ±130) Ma ago based on the Pb-Pb dating on pyritos, which suggests the greenstone-type gold deposit formed after the wall rocks. It can be concluded that the enrichment mineralization depends on shear deformation mobilization.
【Fund】: 国家重点黄金科技攻关项目!90051-01-6-2;;中国科学院广州地球化学研究所所长基金
【CateGory Index】: P595
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