The tectonic links between Palaeozoic eclogites and mafic magmatic Cu-Ni-Co mineralization in East Kunlun orogenic belt, western China | |
Zhang, Mingjie1; Liu, Yuegao2; Chen, Anping3; Liang, Kaikang1; Yang, Yan1; Xu, Wenbo1 | |
刊名 | INTERNATIONAL GEOLOGY REVIEW |
2021-03-05 | |
页码 | 21 |
关键词 | The tectonic settings Cu-Ni-Co mineralization eclogite mafic-ultramafic intrusions the East Kunlun orogenic belt China |
ISSN号 | 0020-6814 |
DOI | 10.1080/00206814.2021.1885504 |
英文摘要 | The Palaeozoic mafic-ultramafic complexes hosting Ni-Cu-Co mineralization occurred discontinuously and coexisted with early Palaeozoic eclogites in the East Kunlun orogenic belt (EKOB), western China. The giant Xiarihamu Cu-Ni-Co sulphide deposit in the EKOB is the largest Cu-Ni-Co sulphide deposit in an orogenic setting in the world. Early Palaeozoic eclogites are distributed as a belt for ca. 530 km in length in the Central Kunlun Zone of the EKOB. The geochronological data, geology and geochemistry of mafic-ultramafic complexes and eclogites in the EKOB are summarized for the tectonic settings of magmatic Cu-Ni-Co mineralization under the Proto- and Paleo-Tethys evolution. The mafic-ultramafic complexes show diverse lithofacies with different formation ages, indicating the multiple stages of long-lived Palaeozoic mantle-derived magmatism in the EKOB. The tectonic location, Neoproterozoic Ocean island basalt (OIB)-like mafic volcanic rocks and eclogite protolith of the EOKB imply the presence of the Neoproterozoic mantle plume magmatism as well as its contribution for enrichments of Ni-Cu-Co beneath EKOB. The ultramafic complexes show a close spatio-temporal relationship with eclogites. The basaltic protoliths of EKOB eclogite were derived from same mantle source as the mafic-ultramafic complexes. A positive correlation of geochronological data between ultramafic complexes with the eclogites in the EKOB is determined and indicated that the mafic magmatism with Cu-Ni-Co mineralization and eclogites were related to the tectonic-magmatic events in process of Proto-Tethys. The ultramafic complexes were formed under the subduction compression and post-collisional extensional settings of the Proto-Tethys and Paleao-Tethys Ocean corresponding to the peak (430-450 Ma) and retrograde (similar to 405-410 Ma) metamorphic periods of eclogites. The Cu-Ni-Co metals were enriched extremely in the stage magma chamber by multi-stage magmatism in EKOB. Therefore, the mafic-ultramafic complexes with a large age span co-occurred with eclogites (especially retrograde eclogites) could be a favourable area for Ni-Co mineralization. |
资助项目 | National Natural Science Foundation of China[91962212] ; National Natural Science Foundation of China[41872075] ; National Natural Science Foundation of China[41873053] ; National Natural Science Foundation of China[41372095] ; STEP[2019QZKK0704] |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | TAYLOR & FRANCIS INC |
WOS记录号 | WOS:000625519100001 |
资助机构 | National Natural Science Foundation of China ; STEP |
内容类型 | 期刊论文 |
源URL | [http://ir.idsse.ac.cn/handle/183446/8566] |
专题 | 深海科学研究部_深海极端环境模拟研究实验室 |
通讯作者 | Zhang, Mingjie |
作者单位 | 1.Lanzhou Univ, Sch Earth Sci, Gansu Key Lab Mineral Resources Western China, Lanzhou, Peoples R China 2.Chinese Acad Sci, Inst Deep Sea Sci & Engn, CAS Key Lab Expt Study Deep Sea Extreme Condit, Sanya, Peoples R China 3.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, Mingjie,Liu, Yuegao,Chen, Anping,et al. The tectonic links between Palaeozoic eclogites and mafic magmatic Cu-Ni-Co mineralization in East Kunlun orogenic belt, western China[J]. INTERNATIONAL GEOLOGY REVIEW,2021:21. |
APA | Zhang, Mingjie,Liu, Yuegao,Chen, Anping,Liang, Kaikang,Yang, Yan,&Xu, Wenbo.(2021).The tectonic links between Palaeozoic eclogites and mafic magmatic Cu-Ni-Co mineralization in East Kunlun orogenic belt, western China.INTERNATIONAL GEOLOGY REVIEW,21. |
MLA | Zhang, Mingjie,et al."The tectonic links between Palaeozoic eclogites and mafic magmatic Cu-Ni-Co mineralization in East Kunlun orogenic belt, western China".INTERNATIONAL GEOLOGY REVIEW (2021):21. |
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