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	Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block; Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block
	HUANG Jie ; ZHANG Cong ; YANG Jingsui ; CHEN Mei ; SHENG Tingting
	2015
关键词	facies orogenic assemblage enough compositional garnet metamorphic minerals variance typically facies orogenic assemblage enough compositional garnet metamorphic minerals variance typically
英文摘要	1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure(P)–temperature(T)and compositional(X)space.In particular,amphibolite facies mafic rocks typically contain similar assemblages:hornblende,plagioclase and epidote,This common assemblage is not enough to calculate the temperature and pressure.However,the existence of Al-rich minerals; 1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure(P)–temperature(T)and compositional(X)space.In particular,amphibolite facies mafic rocks typically contain similar assemblages:hornblende,plagioclase and epidote,This common assemblage is not enough to calculate the temperature and pressure.However,the existence of Al-rich minerals; 大陆构造与动力学国家重点实验室; 2; Vol.89
语种	英语
出处	IGCP649-2015祁连山蛇绿岩野外研讨会
内容类型	其他
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/480088]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	HUANG Jie,ZHANG Cong,YANG Jingsui,et al. Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block, Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyingchi Complex of the Lhasa Block. 2015-01-01.

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