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Petrogenesis of peridotites in the Dargai Complex ophiolite, Indus Suture Zone, Northern Pakistan: Implications for two stages of melting, depletion, and enrichment of the Neo-Tethyan mantle

文献类型:期刊论文

作者Zaheen Ullah; Asad Khan; Shah Faisal; Tehseen Zafar; Huan Li; Muhammad Farhan
刊名Lithos
出版日期2022
卷号426–4277页码:106798
DOI10.1016/j.lithos.2022.106798
URL标识查看原文
语种英语
源URL[http://ir.gyig.ac.cn/handle/42920512-1/13827]  
专题地球化学研究所_矿床地球化学国家重点实验室
作者单位1.Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
2.Department of Geosciences, University of Baltistan Skardu, Skardu 16100, Pakistan
3.Department of Geology, FATA University, Tribal Subdivision Darra, Kohat 26100, KP, Pakistan
4.National Centre of Excellence in Geology, University of Peshawar, Peshawar 25120, KP, Pakistan
5.School of Earth and Space Science, Peking University, Beijing 100871, China
6.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
7.Marine Science Department, Zhejiang University, Zhoushan 316021, China
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Zaheen Ullah,Asad Khan,Shah Faisal,et al. Petrogenesis of peridotites in the Dargai Complex ophiolite, Indus Suture Zone, Northern Pakistan: Implications for two stages of melting, depletion, and enrichment of the Neo-Tethyan mantle[J]. Lithos,2022,426–4277:106798.
APA Zaheen Ullah,Asad Khan,Shah Faisal,Tehseen Zafar,Huan Li,&Muhammad Farhan.(2022).Petrogenesis of peridotites in the Dargai Complex ophiolite, Indus Suture Zone, Northern Pakistan: Implications for two stages of melting, depletion, and enrichment of the Neo-Tethyan mantle.Lithos,426–4277,106798.
MLA Zaheen Ullah,et al."Petrogenesis of peridotites in the Dargai Complex ophiolite, Indus Suture Zone, Northern Pakistan: Implications for two stages of melting, depletion, and enrichment of the Neo-Tethyan mantle".Lithos 426–4277(2022):106798.

入库方式: OAI收割

来源:地球化学研究所

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