阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据

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	刘兆; 仝来喜
	阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据
Source Publication	岩石学报
ISSN	1000-0569
	2015
Volume	31 Issue:6 Pages:1761-1773
Language	中文
Indexed By	SCI
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/31783
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	刘兆,仝来喜. 阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据[J]. 岩石学报,2015,31(6):1761-1773.
APA	刘兆,&仝来喜.(2015).阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据.岩石学报,31(6),1761-1773.
MLA	刘兆,et al."阿尔泰造山带晚古生代高温变质作用与塔里木地幔柱活动的成因联系: 来自泥质和镁铁质麻粒岩的证据".岩石学报 31.6(2015):1761-1773.

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