Abstract：The Baiyinnuoer Pb-Zn deposit in Inner Mongolia is a typical skarn type deposit. However, there is little research concerned with geochemistry and metallogenic dynamics of the ore-forming body. The granitoid rocks that related to mineralization are studied in this article. The results show that the granitoids are high-K calc-alkaline series with enriched LREE and large-ion lithophile elements(LILE) and depleted high field strength elements(HFSE). The origin of magma is the enriched mantle. The mineralization occurred in the post-orogenic extension environment.
杨帆, 汪岩, 付俊彧, 那幅超, 张广宇, 孙巍, 时溢, 张丽. 内蒙古白音诺尔铅锌矿床岩石地球化学特征及地质意义[J]. 地质与资源, 2016, 25(3): 254-260.
YANG Fan, WANG Yan, FU Jun-yu, NA Fu-chao, ZHANG Guang-yu, SUN Wei, SHI Yi, ZHANG Li. GEOCHEMICAL CHARACTERISTICS AND GEOLOGICAL IMPLICATION OF THE BAIYINNUOER Pb-Zn DEPOSIT IN INNER MONGOLIA. GEOLOGY AND RESOURCES, 2016, 25(3): 254-260.
2016, Vol. 25 
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