Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite

doi:10.1016/j.oregeorev.2017.10.026

	Jin, Chang 1,2; Gao, Xin-Yu 1; Chen, Wei Terry 3; Zhao, Tai-Ping 1
	Magmatic-hydrothermal evolution of the Donggou porphyry Mo deposit at the southern margin of the North China Craton: Evidence from chemistry of biotite
Source Publication	ORE GEOLOGY REVIEWS
ISSN	0169-1368
	2018
Volume	92 Pages:84-96
DOI	10.1016/j.oregeorev.2017.10.026
Language	英语
WOS Research Area	Geology ; Mineralogy ; Mining & Mineral Processing
WOS ID	WOS:000424185700007
Indexed By	SCI
Citation statistics	Cited Times:34[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://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
Corresponding Author	Zhao, Tai-Ping
Affiliation	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
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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