Near - west - east thrust fault system and north - south slide fault system resulted from the system separate the west area into different chess - type structural blocks .

Accordingto different shapes,they can be divided into 3 types: the eastern thrust nappe belt,the central thrust fold belt and the western compressive nappe belt.

Research on Majiaheba thrust fault in Leibo of Sichuan;

A study on mechanical mechanism on development of thrust fault;

Geological characteristics of Wengeng thrust fault in Langshan area of western Inner Mongolia

Characteristics of overthrust structures on northern edge of East Qinling-Dabie orogenic belt and hydrocarbon potentials;

The strongly fractured layers overthrust from southeast to northwest, which is proved through tensile fractures and boudins in the layers.

At the same time,tectonic evolution experienced ocean crust diving-collision and intense orogenesis stage,weakly compressing occlude instant volcanic action stage and revived strongly thrust stage,generating many thrust faults to influence sedimentation and denudation and control formation and evolution of thrust belt.

They are characteri zed by thrust and southward dip.

Yingjisu subsidence of the Meso - Cenozoic was a piggyback foreland basin that developed on the base of fold - thrust belts of the Paleozoic.

Fluid veins widely developed in the Daqingshan thrust-nappe,and can be divided into filled veins and edged veins according to their occurrences.

The paper discusses mainly the distribution, geometric features and genesis of thrust structures in Xuyangqiao-Heilongcun buried hill belt in Huanghua depression and the significance in discovering them.

In the northwestern part of North China Craton, there is a series of the Early Proterozoic thrust structures.