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    中国百强科技报刊

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    Volume 33 Issue 1
    Jan.  2008
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    Article Contents
    XIA Qing-lin, ZHAO Peng-da, CHEN Yong-qing, CHENG Qiu-ming, ZHOU Yun-man, 2008. Ni-Mo-V-PGE Mineralization in the Lower Cambrian Black Shale Series from the Deze Area, Yunnan Province, Southwest China. Earth Science, 33(1): 67-73.
    Citation: XIA Qing-lin, ZHAO Peng-da, CHEN Yong-qing, CHENG Qiu-ming, ZHOU Yun-man, 2008. Ni-Mo-V-PGE Mineralization in the Lower Cambrian Black Shale Series from the Deze Area, Yunnan Province, Southwest China. Earth Science, 33(1): 67-73.

    Ni-Mo-V-PGE Mineralization in the Lower Cambrian Black Shale Series from the Deze Area, Yunnan Province, Southwest China

    • Received Date: 2007-04-28
    • Publish Date: 2008-02-25
    • The Qiongzhusi Formation black shale series of the Deze area are located in the western part of the Lower Cambrian black shale zone widely distributed along the southern margin of the Yangtze block, SW China. Different from the Niutitang Formation of black shale in Hunan and Guizhou provinces, the Qiongzhusi Formation contains two distinct metal-rich layers, with V, U, Ag and Pd enriched in the bottom of black carbonaceous siltstones of the lower Shiyantou Section, and Mo, Ni, Pt and Pd in the bottom of black shales of the Yu'anshan Section. In general, the Qiongzhusi Formation is characterized by the enrichment of V-Ni-Mo-U-Ag-Pt-Pd assemblages, whereas the Niutitang Formation is featured with the enrichment of Ni-Zn-Co-Pt-Pd-Ag-Pb association. However, both areas share similar depositional and diagenetic environment (oxegen-reduction) and have similar mechanism for Ni-Mo-PGE mineralization. Ni-Mo-V-PGE mineralization in black shale series is an unconventional type of mineral resources, and it is of great importance to the deposit study and mineral exploitation.

       

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