Jurassic reservoir of Ma lake depression in Jungger basin, Xinjiang;

Topographic ramp often come into being in the edge of depression lake basin in the process of basin basement deformation under extrusion stress, the key factors controlling sequence development such as subsiding rate of basement and initial topographic slope have apparent difference on the two sides of ramp, which in.

The paper chose J1s-K1q1 formation in Shinan area, central Jungar basin asresearch object, which was typical gentle slope of depression lake basin andconducted sequence stratigraphic research, depositional facies research and oil poolforming rules research.

Sequence stratigraphy of Quaternary Seven Spring Group of the Sanhu depression and prediction for prospective targets for hydrocarbons;

The Pliocence—Quaternary System self-source and self-reservoir natural gas reservoir of the Sanhu Depression lie in the east Qaidam Basin that has become one of the biggest four natural gas producing districts.

Temporal and Spatial Configuration of Sedimentary Systems and Sequence Stratigraphic Framework of Sangonghe Formation in Bohu Depression of Yanqi Basin;

Study on crop, single well sequence and sedimentology of Badaowan formation in Bohu depression;

High Precision Sequence Stratigraphic Analysis of Single Well in Bohu Depression;

Significance of slope break zones in downwarped lake basins to exploration of non-structural traps in Junggar basin;

Characteristics of slope breaks and their control on atectonic traps in downwarped lake basin;

Research on Seismic Stratigraphy and Petroleum Geology of the Permian in Mahu Depression of Junggar Basin;