| Discovery of the Archean Magmatic Cu-Ni Sulfide Deposit in China—Taoke Deposit,Shandong Province |
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| 作者姓名： | SUN Tao WANG Denghong LI Chao ZHANG Zengqi SUN Bin CHENG Wei LI Wanting ZHANG Aiping |
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| 作者单位： | School of Earth Sciences;MNR Key Laboratory of Metallogeny and Mineral Assessment;National Research Center for Geoanalysis;Shandong Institute of Geological Sciences |
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| 基金项目： | the National Science Foundation of China(41862005,41872089 and 41702091);Yunnan Applied Basic Research Project(2018FB079);China Geological Survey(DD20160346). |
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| 摘 要： | The formation ages of global magmatic sulfide Ni-Cu deposits are from Archean to Mesozoic,the Neoarchean and Neoproterozoic are the two peaks.In China,the formation ages of magmatic sulfide deposits are from Proterozoic to Mesozoic,and the Neoproterozoic and late Paleozoic are the two peaks,.Compared with the global magmatic deposits,there is no case study of the Archean magmatic Ni-Cu sulfide deposits in China before.The nickel deposits formed in Neoproterozoic are located on the margin of the North China Block and Yangtze Block(e.g.Jinchuan,Dapoling),and those formed in the late Paleozoic are mainly distributed in the Central Asian Orogenic Belt(CAOB).Emeishan and Tarim Large Igneous Provinces(LIPs).such as Kalatongke,Yangliuping,and Pobei.
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| 关 键 词： | MAGMATIC MESOZOIC ARCHEAN |
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