supported by the National Key Research and Development Program of China from the Ministry of Science and Technology of China(Grant No.2017YFC0601301);the National Natural Science Foundation of China(Grant Nos.41772232 and 41830216);the Projects of the China Geological Survey(Grant Nos.DD20190358 and DD20190001)。
Many orogenic belts in the world exhibit accretionary and collisional orogenic phases to varying extents.How accretion evolves into collision of the Central Asian Orogenic Belt(CAOB),the largest Phanerozoic accretiona...
financially supported by the National Science and Technology Major Project (No.2011ZX05008-001);the Natural Science Foundation of China (No.40739906);the Chinese State 973 Project(No. 2011CB201100)
The Wulungu Depression is the northernmost first-order tectonic unit in the Junggar Basin. It can be divided into three sub-units: the Hongyan step-fault zone, the Suosuoquan sag and the Wulungu south slope. The Ceno...
financially supported by the National Science and Technology Major Project(Grant No.2011ZX05008-001);the National Natural Science Foundation of China(Grant No.40739906);the Chinese State 973 Project(Grant No.2011CB201100)
The Hala'alat Mountains are located at the transition between the West Junggar and the Junggar Basin. In this area, rocks are Carboniferous, with younger strata above them that have been identified through well data ...
financially supported by the Chinese National Basic Research 973 Program(2012CB416604,2007CB411307);the National Natural Science Foundation of China(41230207,41390441,41190075);the One Hundred Talent Program B of the Chinese Academy of Sciences
How ophiolitic mèlanges can be defined as sutures is controversial with regard to accretionary orogenesis and continental growth.The Chinese Altay,East junggar,Tianshan,and Beishan belts of the southern Central Asian...