Comparing of the tectonic uplift since Late Cenozoic between the East and West Kunlun Mountains;

There is a very well-developed fault system in the western sector of the East Kunlun, and thrust propagation, normal slip and decoupling were the main deformation events in the area; 2.

Study shows that the Meso-and Neopro terozoic volcanic rocks distributed south of the line of Cele-Mingfeng-Yutian on the northern margin of the eastern segment of the West Kunlun Mountains ,Xinjiang,consist dominantly of a suite of low-grade(basaltic)andesite with very small amount of rhyolite.

A sequence of paralic strata which contains biota fossils from Early-Middle Devonian is found in Bukadaban district in west-middle section of East Kunlun Mt.