摘要
A large area of Late Paleozoic intrusions occursalong the Kalamaili fault in North Xinjiang,which is divided into I-type and A-type granite(Liu et al.,2013),and are the ideal objects for revealing the geological evolution of this region.However,the study of the granodioritic pluton in East Junggar is particularly weak.
基金
supported financially by the NSFC projects(Grant Nos.U1403291,41830216,and 41802074)
projects of the China Geological Survey(Grant Nos.DD20160024,DD20160123,and DD20160345)
IGCP 662.
