GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 期刊论文
Jin, Chang1,2; Gao, Xin-Yu1; Chen, Wei Terry3; Zhao, Tai-Ping1
Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite
Source PublicationORE GEOLOGY REVIEWS
Corresponding AuthorZhao, Tai-Ping(tpzhao@gig.ac.cn)
ISSN0169-1368
2018
Volume92Pages:84-96
DOI10.1016/j.oregeorev.2017.10.026
Indexed BySCI
Language英语
WOS Research AreaGeology ; Mineralogy ; Mining & Mineral Processing
WOS IDWOS:000424185700007
Funding OrganizationNational Key Research and Development Program of China ; National Natural Science Foundation of China ; Thousand Youth Talents Plan grant
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Cited Times:7[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/36881
Collection中国科学院矿物学与成矿学重点实验室_期刊论文
Corresponding AuthorZhao, Tai-Ping
Affiliation1.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
Recommended Citation
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.
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