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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

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

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Supported by the Projects of Sanya Yazhou Bay Science and Technology City of Hainan Province (2021CXLH0027) and National Key Research and Development Project (2019YFC0605201).

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  • Available Online: February 03, 2024
  • [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. [Methods]The 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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