Through seismic stratigraphic analysis on the northern area of Hami Basin, it is thought that there developed a set of alluvial fan fan delta shal low loch deposit system from north to south in the lower part of Badaowan format ion in Jurassic.

Surrounded by the llarkol Mountains, Karlik Mountains and Qoltag Mountains, Hami Basin is a large intermontane basin in the eastern part of the Tianshan Mountains.

Lies in the eastern Xinjiang,the Turpan-Hami Basin is one of the three most important large oil-enriched basins in Xinjiang district.

The Upper Permian, Triassic and Jurassic strata in the Turpan Hami basin have a wide distribution of alluvial fan, fluviolacustrine deposit, fan delta, braided delta and normal delta deposit, which are most characterized by the fan delta and braided delta deposits whose skeletons are mainly channel sandbodies.

Based on the theory of sequence stratigraphy,the sequence features of the Jurassic at the southern margin of Tulufan-Hami Basin have been analyzed and three type of I sequences have been identificated approximately corresponding to Badaowan,Sangonghe and Xishanyao Formations respectively.

Flow Unit Classification of Mid-Jurassic Reservoir in Qiudong Condensate Gas Reservoir,Tuha Basin;

Development characteristics and geneses of the fractures in low-permeability sandstone reservoir in the nothern depression of Tuha Basin;

Logging Interpreting Method Used for Extra-low Permeability Reservoirs in Tuha Basin;

Analysis of Middle-Jurassic seismic facies in Hongtai area of Tu-Ha basin;

Characteristics of element geochemistry of Shuixigou Group in north-eastern Tu-Ha Basin;

Discussion on reservoir prediction and reservoir-accumulating feature in Putaogou area of Tu-Ha basin;