Multi-stage crustal melting from Late Permian back-arc extension through Middle Triassic continental collision to Late Triassic post-collisional extension in the East Kunlun Orogen | |
Xu Zhao; Junhao Wei; Lebing Fu; Jan Marten Huizeng; M. Santosh; Jiajie Chen; Dianzhong Wang; Aobing Li | |
2020 | |
Source Publication | Lithos
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Volume | 360-361Pages:105446 |
DOI | 10.1016/j.lithos.2020.105446 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gyig.ac.cn/handle/42920512-1/11771 |
Collection | 矿床地球化学国家重点实验室 |
Affiliation | 1.School of Earth Resources, China University of Geosciences, Wuhan 430074, China 2.Economic Geology Research Institute (EGRU), College of Science and Engineering, James Cook University, Townsville, Queensland 4811, Australia 3.Department of Geology, University of Johannesburg, PO Box 524, Auckland Park 2006, South Africa 4.School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China 5.Department of Earth Sciences, University of Adelaide, Adelaide, SA 5005, Australia 6.Yonsei Frontier Lab, Yonsei University, Seoul, Republic of Korea 7.School of Earth Science, East China University of Technology, Nanchang 330013, China 8.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China |
Recommended Citation GB/T 7714 | Xu Zhao,Junhao Wei,Lebing Fu,et al. Multi-stage crustal melting from Late Permian back-arc extension through Middle Triassic continental collision to Late Triassic post-collisional extension in the East Kunlun Orogen[J]. Lithos,2020,360-361:105446. |
APA | Xu Zhao.,Junhao Wei.,Lebing Fu.,Jan Marten Huizeng.,M. Santosh.,...&Aobing Li.(2020).Multi-stage crustal melting from Late Permian back-arc extension through Middle Triassic continental collision to Late Triassic post-collisional extension in the East Kunlun Orogen.Lithos,360-361,105446. |
MLA | Xu Zhao,et al."Multi-stage crustal melting from Late Permian back-arc extension through Middle Triassic continental collision to Late Triassic post-collisional extension in the East Kunlun Orogen".Lithos 360-361(2020):105446. |
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