The Ophiolitic Mélanges in Strike-slip Fault Zones in West Junggar, Xinjiang, NW China

CORC > 北京大学 > 地球与空间科学学院

	The Ophiolitic Mélanges in Strike-slip Fault Zones in West Junggar, Xinjiang, NW China
	GUO Zhaojie ; CHEN Shi ; ZHANG Yuanyuan
刊名	Acta Geologica Sinica(English Edition)
	2017
关键词	Carboniferous ocean sedimentary strike collision sandstone NW China Xinjiang crust zircon
英文摘要	The West Junggar region of western China,located in the far eastern end of the Kazakhstan orocline,occupies the junction of the Siberia,Tarim and Kazakhstan blocks,which is crucial for palinspastic reconstruction of the CAOB.The principal rock assemblages in West Junggar include Paleozoic ophiolitic mélanges and a thick,undeformed Upper Devonian–Lower Carboniferous sedimentary succession as the boundary of the mélanges,both of which are intruded by sub-circular Upper Carboniferous granitoid plutons and inte; S1; 13-14
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/479646]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	GUO Zhaojie,CHEN Shi,ZHANG Yuanyuan. The Ophiolitic Mélanges in Strike-slip Fault Zones in West Junggar, Xinjiang, NW China[J]. Acta Geologica Sinica(English Edition),2017.
APA	GUO Zhaojie,CHEN Shi,&ZHANG Yuanyuan.(2017).The Ophiolitic Mélanges in Strike-slip Fault Zones in West Junggar, Xinjiang, NW China.Acta Geologica Sinica(English Edition).
MLA	GUO Zhaojie,et al."The Ophiolitic Mélanges in Strike-slip Fault Zones in West Junggar, Xinjiang, NW China".Acta Geologica Sinica(English Edition) (2017).