中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Marine Carbonate Component in the Mantle Beneath the Southeastern Tibetan Plateau: Evidence From Magnesium and Calcium Isotopes

文献类型:期刊论文

作者Liu, Fang1,2; Li, Xin1; Wang, Guiqin1; Liu, Yufei1,2; Zhu, Hongli1,2; Kang, Jinting1,3; Huang, Fang3; Sun, Weidong4,5; Xia, Xiaoping1; Zhang, Zhaofeng1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2017-12-01
卷号122期号:12页码:9729-9744
ISSN号2169-9313
DOI10.1002/2017JB014206
通讯作者Zhang, Zhaofeng(zfzhang@gig.ac.cn)
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000423129200046
资助机构Chinese Academy of Sciences ; National Natural Science Foundation of China ; State Key Laboratory of Geological Processes and Mineral Resources
源URL[http://ir.gig.ac.cn/handle/344008/34982]  
专题同位素地球化学国家重点实验室
通讯作者Zhang, Zhaofeng
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Guangdong, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Univ Sci & Technol China, Sch Earth & Space Sci, Key Lab Crust Mantle Mat & Environm, Hefei, Anhui, Peoples R China
4.Chinese Acad Sci, Inst Oceanog, Ctr Deep Sea Res, Qingdao, Peoples R China
5.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Liu, Fang,Li, Xin,Wang, Guiqin,et al. Marine Carbonate Component in the Mantle Beneath the Southeastern Tibetan Plateau: Evidence From Magnesium and Calcium Isotopes[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2017,122(12):9729-9744.
APA Liu, Fang.,Li, Xin.,Wang, Guiqin.,Liu, Yufei.,Zhu, Hongli.,...&Zhang, Zhaofeng.(2017).Marine Carbonate Component in the Mantle Beneath the Southeastern Tibetan Plateau: Evidence From Magnesium and Calcium Isotopes.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,122(12),9729-9744.
MLA Liu, Fang,et al."Marine Carbonate Component in the Mantle Beneath the Southeastern Tibetan Plateau: Evidence From Magnesium and Calcium Isotopes".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 122.12(2017):9729-9744.

入库方式: OAI收割

来源:广州地球化学研究所

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