First arrival seismic tomographic imaging test of the near-surface velocity structure of central uplift in the Qiangtang basin,Qinghai-Tibet Plateau

Study of Structure and Pool-forming Condition of Dongying Formation in the Central Uplift of Dongying Sag;

Fault systems in the Central uplift of the Dongying depression are complex.

The northern one is called the Yimeng paleouplift, and the south-central one, the Central paleouplift.

To reveal the formation mechanism of the Carboniferous slender-waist-shaped central paleouplift in Ordos Basin,a series of stress-strain simulations were carried out,in which the basin was simplified into an isopachic,isotropic and elastic shell model and loaded with the NS trending extrusion.

The authors think that the central paleouplift in the Ordos basin was formed under the nearly E W lateral compressive stress produced by the collision and amalgamation of the Qilian trough and the Ordos basin in early Palaeozoic time.

Quantitative study of the influence of structural adjustments on the accumulation and distribution of petroleum in central uplift belt,Tarim basin;

Potential areas and exploration direction in the central uplift belt of the Tarim Basin;

An analysis of oil-source characteristics of central uplift belt in Dongying depression;

Deep-seated structural characteristic and evolution of paleo-central uplift belt in northern Songliao basin;

The Process of Structure-sedimentary and Their Correlation of the Cambrian Peroid in the Central Uplift Belt, Tarim Basin;

Structural features of the central uplift belt have been investigated by basin analysis and accommodation zone theory,indicating that,uplift forming has been controlled by the second grade faults,local structure has been controlled and complicated by the third and forth grade faults,and oil-gas accumulation level has been controlled by the combination features of faults.