Discovery of the Gravity Gliding Tectonic of Shanwang Formation,Shanwang Basin;

s: With the typical sequence stratigraphic theories the sequence stratigraphic correlation between Shanwang Formation in Shanwang basin and upper Guantao Formation in Jiyang depression are performed.

The Shanwang Basin is located at 36°N,118°E,and is an interior lake basin of middle Miocene age which contains abundant plant and animal fossils.

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;

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.

Located in a tectonic uplift region in Zixi county, Jiangxi province, the Fashui hot spring along the Erkou Shixia fault belt is a typical intermountain basin type hot spring with a geothermal anormaly area less than 1km 2.