中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite

文献类型:期刊论文

作者Jin, Chang1,2; Gao, Xin-Yu1; Chen, Wei Terry3; Zhao, Tai-Ping1
刊名ORE GEOLOGY REVIEWS
出版日期2018
卷号92页码:84-96
ISSN号0169-1368
DOI10.1016/j.oregeorev.2017.10.026
通讯作者Zhao, Tai-Ping(tpzhao@gig.ac.cn)
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000424185700007
资助机构National Key Research and Development Program of China ; National Natural Science Foundation of China ; Thousand Youth Talents Plan grant
源URL[http://ir.gig.ac.cn/handle/344008/36881]  
专题中国科学院矿物学与成矿学重点实验室
通讯作者Zhao, Tai-Ping
作者单位1.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Guangdong, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100039, Peoples R China
3.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Guizhou, Peoples R China
推荐引用方式
GB/T 7714
Jin, Chang,Gao, Xin-Yu,Chen, Wei Terry,et al. Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite[J]. ORE GEOLOGY REVIEWS,2018,92:84-96.
APA Jin, Chang,Gao, Xin-Yu,Chen, Wei Terry,&Zhao, Tai-Ping.(2018).Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite.ORE GEOLOGY REVIEWS,92,84-96.
MLA Jin, Chang,et al."Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite".ORE GEOLOGY REVIEWS 92(2018):84-96.

入库方式: OAI收割

来源:广州地球化学研究所

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