东准噶尔扎河坝超高压变质成因石英菱镁岩的40Ar/39Ar同位素年代学信息及地质意义

GIG OpenIR > 中科院广州地化所(-2008)

	牛贺才; 单强; 张海祥; 于学元
	东准噶尔扎河坝超高压变质成因石英菱镁岩的40Ar/39Ar同位素年代学信息及地质意义
Source Publication	岩石学报
ISSN	1000-0569
	2007
Volume	23 Issue:7 Pages:1627-1634
Language	中文
Indexed By	sci
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/13593
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	牛贺才,单强,张海祥,等. 东准噶尔扎河坝超高压变质成因石英菱镁岩的40Ar/39Ar同位素年代学信息及地质意义[J]. 岩石学报,2007,23(7):1627-1634.
APA	牛贺才,单强,张海祥,&于学元.(2007).东准噶尔扎河坝超高压变质成因石英菱镁岩的40Ar/39Ar同位素年代学信息及地质意义.岩石学报,23(7),1627-1634.
MLA	牛贺才,et al."东准噶尔扎河坝超高压变质成因石英菱镁岩的40Ar/39Ar同位素年代学信息及地质意义".岩石学报 23.7(2007):1627-1634.

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