Chen M H, Shi L. Filling and evolution of the Late Paleozoic Shuicheng-Ziyun aulacogen in western Guizhou, China. Geological Bulletin of China,;

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.

Recognition of Buried Aulacogen and Hydrocarbon Potential in Qiangtang Area of Qinghai-Tibet Plateau.;

According to the ecologic and sedimentary features, the Late Permian biota and strata of south Guizhou can be grouped into the “shallow platform type”and “sub byssal aulacogen type”.

On the basis of the division, correlation and study of the framework of sequences in the stable regions and rift trough in the Luofu, Dachang sections, Nandan County,the formati.