From a quantitative and semi-quantitative research on Fenwei rift valley system,we suggest that basin-mountain dichotomy of the rift valley system was formed under a regional extensional stress field.

Evaluation of geochemical characteristics of hydrocarbon source rock and gas-generating potential in Upper Tertiary, Baoshan Basin;

Time-space distribution of the sands in the third member of Yangyi formation,Yongzhujie uplift,Baoshan Basin;

Biological Gas Resource and its Exploration Potential in Neogene,Baoshan Basin;

Structural feature and basin-mountain coupling analysis of North Sichuan Basin;

Recently, the research of basin-mountain coupling has become one of the hotspots in Geology.

The relationship between basin-mountain coupling process and metallogeny is a hot spot in modern geological research.

Integrating study the relationship between basin-mountain system and oil and gas pool forming process is one of the frontier research fields in the study of continental geodynamics,and also is a key problem of petroleum exploration in China.

Therefore, analysis of the architecture and tectonic evolution of the basin-mountain system in Sichuan Basin and its adjacent areas would be very important to gain a deeper understanding of the tectonic framework of and petroleum reservoir distribution in Sichuan basin.

The distributing character of the magnetic structure was inverse at the different depth of Xiangshan basin.

Strike-slip pull-apart process and emplacement of Xiangshan uranium-producing volcanic basin;

Geological conditions for ore-forming process and prospecting direction of the U-Mo polymetallic deposits in Guyuan volcanic basin;

Lingquan volcanic basin is located in the mid-southern segment of known Rrguna-Kelulun Eastnorth-trending volcanic rocks uranium metallogenic belt,it is on the same belt with Telechuf Field of Russia and Durnuot Field of Mongolia.