辉石岩:高压结晶还是再循环洋壳?

GIG OpenIR

	张亚玲; 徐义刚
	辉石岩:高压结晶还是再循环洋壳?
Source Publication	高校地质学报
ISSN	1006-7493
	2012
Volume	18 Issue:1 Pages:74-87
Indexed By	CSCD
Language	中文
CSCD ID	CSCD:4502596
Citation statistics	Cited Times:3[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/17873
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	张亚玲,徐义刚. 辉石岩:高压结晶还是再循环洋壳?[J]. 高校地质学报,2012,18(1):74-87.
APA	张亚玲,&徐义刚.(2012).辉石岩:高压结晶还是再循环洋壳?.高校地质学报,18(1),74-87.
MLA	张亚玲,et al."辉石岩:高压结晶还是再循环洋壳?".高校地质学报 18.1(2012):74-87.

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