The conclusions are as follows: the Balihan detachment fault was the main controlling fault;during the earlier period,Pingzhuang basin was a graben basin but in middle and later period,the basin became a semi-graben basin;the extrusing tectonic stress field made Pingzhuang rift basin died out;since then this area underwent str.

Sequence stratigraphy and coal-forming laws in Pingzhuang basin of Inner Mongolia;

ANSYS-based numeric simulation of ground temperature field in north of Pingzhuang basin;

Low-medium temperature geothermal system of connective type and target zone of exploration in Pingzhuang basin;

The law of basement pre-existing fabric controlling fault formation and evolution in rift basin

The meso Tethys was formed and extended during the Late Triasso Jurassic,when in the Nyalam area of southern Tibet there were extensive and corresponding sediments accummulated in the rift basin,as well as numerous extension unconformities.

The Mesozoic-Cenozoic extensional tectonic system in eastern China is composed of rift basins and extensional mountain system.

The coupling relationship between basin and mountains is a frontier hot topic for geoscience today, and it is generally considered that fracture systems serves as the coupling links among tectonic groups, such as between extensional orogenic belts and rifting basins, between compressional orogenic belts and foreland basins, as well as between orogenic belts and strike-slip basins.