峨眉火成岩省内带岩浆硫化物含矿岩体橄榄石的成因意义

	峨眉火成岩省内带岩浆硫化物含矿岩体橄榄石的成因意义
	官建祥; 宋谢炎; Leonid V.Danyushevsky; 陈列锰; 聂晓勇
	2010
Source Publication	地球科学(中国地质大学学报)
Issue	2 Pages:224-234
Keyword	峨眉火成岩省内带岩浆硫化物矿床橄榄石分离结晶硫化物熔离晶间熔浆效应
Subject Area	矿床地球化学
Indexed By	CSCD
Language	中文
CSCD ID	CSCD:3895625
Citation statistics	Cited Times:6[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/6883
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	官建祥,宋谢炎,Leonid V.Danyushevsky,等. 峨眉火成岩省内带岩浆硫化物含矿岩体橄榄石的成因意义[J]. 地球科学(中国地质大学学报),2010(2):224-234.
APA	官建祥,宋谢炎,Leonid V.Danyushevsky,陈列锰,&聂晓勇.(2010).峨眉火成岩省内带岩浆硫化物含矿岩体橄榄石的成因意义.地球科学(中国地质大学学报)(2),224-234.
MLA	官建祥,et al."峨眉火成岩省内带岩浆硫化物含矿岩体橄榄石的成因意义".地球科学(中国地质大学学报) .2(2010):224-234.

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