Mesozoic-Cenozoic structural evolution in Qaidam Basin and its control on hydrocarbon occurrence;

The structural evolution and prospecting direction of the Yichun Pb,Zn(Ag) metallogenic belt;

Inversion structure and structural evolution in Zhoukou depression;

Cenozoic tectonic evolution and hydrocarbon accumulation in Bonan Region;

Mesozoic deformation and tectonic evolution in Chengdao,Southern Bohai Bay;

Meso-Cenozoic tectonic evolution and uranium potential evaluations of basins in Beishan-Gansu Corridor region;

From the point of view about sediment-structures evolution the uneven sediment-structure evolution movement-laws along north-south direction in Longxian region of southwestern Ordos Basin have been found with time clues,and by analyzing and comparing about the thickness of the initial formation and the residual of the Jurassic,Cretaceous and Paleogene system.

Structure evolution of the fracture has controlled the distribution of the major mineral resources on the both sides.

Relationship between Palaeogene tectonic evolvement and development of source rock in the east of China;

Helium isotopic compositions in natural gases have a good relationship with geology tectonic background,which indicate the features of tectonic evolvement in a great region but don't work for a small region in the same basin.

Describe their macro-geometry, micro-geometry and kinematics characteristics, affirm their deep, media, shallow tectonic evolvement.