financially supported by the Projects of the China Geological Survey(Grant No.12120115027001,121201102000150005-06);Natural Science Foundation of China(Grant No.41272079,41302266)
The South Altyn continental block is an important geological unit of the Altyn Tagh orogenic belt, in which numerous Neoproterozoic granitoids crop out. Granitoids are mainly located in the Paxialayidang-Yaganbuyang a...
financially supported by the National Natural Science Foundation of China(No.41502046,41530211 and 41272079)
1 Introduction The Wulong glomerophyric diorite porphyry has an extremely peculiar texture with plagioclase phenocrysts clustered as flower-like glomerocrysts(Figs.1a&b),which is never discovered elsewhere of the worl...
financially supported by the National Nature Science Foundation of China (Grant 41272079)
There is a general consensus that most ophiolites formed above subduction zones(Pearce,2003),particularly during forearc extension at subduction initiation(Shervais,2001;Stern,2004;Whattam and Stern,2011).'Supra-Subdu...