Some uplift zones,formed in this time,are responsible for the reform in late period of the formation of this basin,which especially caused the generation of Jianshan structure zone and the shifting of the center of subsidence in the Moliqing region.

Terrestrial-stress logging responding characteristics of piedmont tectonic belt and its influence on reservoir property;

Tianshan tectonic belt is the most important metallogenetic region of Tianshan large to super-large metallogenetic belt in Tianshan-Xingmeng metallogenetic province in the Central Asia metallogenetic domain,and Bingdaban-Alagou zone is the most favorable one in this region.

Depositional process and evolution of Luanping Early Cretaceous basin in the Yanshan structural belt.;

The Fengshan basin is a well-preserved extensional basin in the Yanshan structural belt.