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    刘月高, 张江伟, 冯志兴, 杨顺龙, 王义忠, 李积清, 赵志逸, 王治安, 李树雷, 陈正国, 王厚方. 青藏高原东北缘岩浆型铜镍钴硫化物矿床勘查模型与研究进展[J]. 中国地质. DOI: 10.12029/gc20230128003
    引用本文: 刘月高, 张江伟, 冯志兴, 杨顺龙, 王义忠, 李积清, 赵志逸, 王治安, 李树雷, 陈正国, 王厚方. 青藏高原东北缘岩浆型铜镍钴硫化物矿床勘查模型与研究进展[J]. 中国地质. DOI: 10.12029/gc20230128003
    LIU Yuegao, ZHANG Jiangwei, FENG Zhixing, YANG Shunlong, WANG Yizhong, LI Jiqing, ZHAO Zhiyi, WANG Zhian, LI Shulei, CHEN Zhengguo, WANG Houfang. Exploration and research progress of magmatic copper-nickel-cobalt sulfide deposits in the north-eastern margin of the Qinghai-Tibetan Plateau[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20230128003
    Citation: LIU Yuegao, ZHANG Jiangwei, FENG Zhixing, YANG Shunlong, WANG Yizhong, LI Jiqing, ZHAO Zhiyi, WANG Zhian, LI Shulei, CHEN Zhengguo, WANG Houfang. Exploration and research progress of magmatic copper-nickel-cobalt sulfide deposits in the north-eastern margin of the Qinghai-Tibetan Plateau[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20230128003

    青藏高原东北缘岩浆型铜镍钴硫化物矿床勘查模型与研究进展

    Exploration and research progress of magmatic copper-nickel-cobalt sulfide deposits in the north-eastern margin of the Qinghai-Tibetan Plateau

    • 摘要:研究目的】为提升我国Cu-Ni-Co资源供应安全,有必要梳理青藏高原东北缘东昆仑造山带的岩浆型铜镍钴硫化物矿床的的成矿规律与找矿标志。【研究方法】本文系统总结了东昆仑地区除蛇绿岩以外的5期基性-超基性侵入杂岩体:晚奥陶世-早志留世、中晚志留世-早中泥盆世、早石炭世、中二叠世-早三叠世、中-晚三叠世的矿物学、岩石学、年代学、地球化学和地球物理特征。【研究结果】在上述工作基础上,本文归纳了岩浆型铜镍矿的源区性质及其与高压-超高压榴辉岩、原-古特提斯演化的关系,分析了地壳硫混染及结晶分异对硫化物饱和影响,提出了矿体优选赋存的位置,对比了成矿岩体与非成矿岩体的代表性差异。【结论】最终本文建立东昆仑造山带岩浆铜镍钴硫化物矿床的综合信息勘查模型。

       

      Abstract: Objective To improve the supply security of Cu-Ni-Co resources in China, it is necessary to sort out the mineralization regularity and prospecting indicators of the magmatic copper-nickel-cobalt sulfide deposit in the Phanerozoic in the Eastern Kunlun orogenic belt on the northern margin of the Qinghai-Tibet Plateau. MethodsThe geological, geochronology, geochemistry, and geophysical characteristics of five stages mafic-ultramafic complexes including the Late Ordovician-Early Silurian, the Middle Silurian-Middle Devonian, the Early Carboniferous, the Middle Permian-Early Triassic, and the Middle-Late Triassic are summarized. Results Based on the above work, the source area properties of magmatic copper-nickel deposits and their relationship with the highpressure-ultrahighpressure eclogite and the evolution of Proto-Paleo Tethys were discussed. The influence of crustal sulfur contamination and crystal differentiation on sulfide saturation was analyzed. The rules of the optimal location of copper-nickel ore bodies were summarized. The typical differences between the ore-forming mafic-ultramafic complexes and the no-ore mafic-ultramafic complexes were described. Conclusions At last, a comprehensive information exploration model was established.

       

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