Under continuous N-S convergence between the Indian and Eurasian continents, the Sichuan-Yunnan block on the southeastern margin of the Tibetan Plateau has undergone southeastward extrusion and clockwise rotation since late Cenozoic along the right-lateral Red River to the southwest and left-lateral Xianshuihe-Xiaojiang Fault systems to the northeast.

Relation between the 2005 Huize M5.3 Earthquake and the Seismicity of Xiaojiang Fault;

Modern activity in the southern and central parts of the Xiaojiang fault in Yunnan;

The middle section of the Xiaojiang fault zone located in Yunnan Province is branched into east and west two faults.

At present,it is facing the main problems of low abundance,small fault,thin sand layer,having complex and levity reservoir and relying mainly on composite structure-lithology reservoir.

Genetic mechanism of the fault system in the Yinggehai basin;

Application of ant colony algorithm in fault system interpretation

Formation mechanism of Cenozoic fault system of Nanpu sag in Bohai Bay Basin

Fault systems in central area of the Tarim Basin:geometry,kinematics and dynamic settings;

As a result,the authors find that these fault systems are statistically self similar within the scale range studied (r=0.

Combined with research of fault systems in structural subarea,the writers divided the southern NCC in Meso—Cenozoic into western Henan basin—ridge area,eastern Henan basin area and Xuzhou—Huainan basin area.