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《Geochimica》 1991-04
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REE GEOCHEMISTRY OF THE JINDING SUPERLARGE Pb-Zn DEPOSIT

Wang Jingbin Li Chaoyang(Institute of Geochemistry, Academia Sinica, Guiyang 550002)  
REE geochemical studies of ores, altered wall rocks and hydrothermal-sedimentary rocks from the Jinding superlarge Pb-Zn deposit, Yunnan Province indicate that the REE patterns in ore fluids are characterized by strong LREE enrichment, with weak (negative and positive) Eu and remarked negative Ce anomalies. In conjunction with isotope and other trace element data, it is suggested that the ore-forming material was' derived mainly from CO2-riched mantle flow in which REE and part of the metals were transported as carbonate-complexes. The ore fluids are weakly alkaline in nature.
【Fund】: 中国科学院矿床地球化学开放实验室
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