Combined with the historical materials,the ancient and near stratums of Pinglu basin,Yuanqu basin,the west of Jiyuan basin had been carried on the characteristic contrast of the stratum of rock and stratum,biological stratum,times stratum through geological survey of Houma and Xinxiang in 1:250 000.

Transporting conditions of faults required in formation of large and medium gas fields with high efficiency in foreland basin;

Different origins of natural gas in secondary gas pool in Western Sichuan foreland basin;

Overpressure compartment sealed by faults in Kuqa foreland basin;

Chimney structures in the shelf basin of East China Sea;

Exploration of subtle reservoirs in the northern shelf basins of South China Sea;

Non-structural reservoirs in northern shelf basins of South China Sea;

Relationship between unconformity system and heterogeneous migration of petroleum in continental basins;

Application prospects of cross well seismic technique to continental basins;

Petroleum Geology and exploration prospects in the Cenezoic continental basins in the northern part of the Qinghai-Xizang Plateau;

Sedimentary characteristics of nearshore subaqueous fan of Neogene Ciying Formation in Luliang basin.Yunnan;

Luliang Basin is a typical representative of Tertiary sedimentary basins in Yunnan Province.

Luliang Basin is a typical representative of the Tertiary sedimentary basins in Yunnan Province.

Discussio on"one divides into four"property of system domain for stratigraphic sequence of terrestrial basins of China and its advantages;

In analysis of imaging stratigraphy for Cretaceous terrestrial basin in Xingjiang,in the light of modern stratigraphic theory,using analysis methods of sequence stratigraphy and tectonic sequence,the recognition marks of imaging sequence interfaces in remote sensing are built, and combined with 1∶50000 geological survey,the interpretating methods of imaging tectonic sequenc are discussed.

On the basis of analyzing the present situation of exploration in fault depressions in terrestrial basins,the conception of generalized sag is proposed,such as the alar part of the steep belt in fault depressions,the major sag,and the mid-lower part of slope belts.