Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment

	Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment
	Xie-Yan Song; Xiang-Ren Li
	2009
Source Publication	Mineralium Deposita
Volume	44 Issue:3 Pages:303-327
Indexed By	SCI
Language	英语
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/4415
Collection	矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation GB/T 7714	Xie-Yan Song,Xiang-Ren Li. Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment[J]. Mineralium Deposita,2009,44(3):303-327.
APA	Xie-Yan Song,&Xiang-Ren Li.(2009).Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment.Mineralium Deposita,44(3),303-327.
MLA	Xie-Yan Song,et al."Geochemistry of the Kalatongke Ni–Cu–(PGE) sulfide deposit, NW China: implications for the formation of magmatic sulfide mineralization in a postcollisional environment".Mineralium Deposita 44.3(2009):303-327.

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