The transgressive systems tract of the continental sepquences in the Biyang fault depression as a lacustrine basin is dominated by a retrogradational fan delta.

According to the facies migration character and superimposed style of systems tract in reference well of Biyang fault depression, the terrigenous sequence in Shuanghe Zhaoao area can be derived into two types (type Ⅰand Ⅱ).

The upper member of Eh 3 of Biyang fault-depression includes three terrigenous sequences(S4,S5 and S6).

Biyang fault-depression experienced three evolutional phases: pullapart during Mesozoic, rift during Paleogene, and downwarping in Neogene.

The basin-forming history in Biyang fault-depression consists of three evolution stages:initial rift(K2),main rift(E) and downwarp(N).

There is great thickness of lake sediments of Eogene in Biyang rifted-basin.

The formation of the complicated reservoir in Biyang rifted-basin is associated with the evolution of thecomplicated deep faults at the south-east boundary of the rifted-basin.

Oil and Gas Enrichment Rules and Analysis on Secondary Exploration Potential in the Noruh Slope of Biyang Depression;

Hydrocarbon Accumulation System and Its Resource Potential in Biyang Depression of Nanxiang Basin;

Deep-Basin Oil Pool of the Zhaowa-Anpeng Field in the Biyang Depression of the Nanxiang Basin;

Sequence stratigraphy and stratum-lithology trap prediction of the Eh_3 upper member of Hetaoyuan Formation in south Xia'ermen Oilfield,Biyang Sag;

Sand reservoir prediction of steep slope zone in Biyang Sag;

Comparative analysis of heavy oil consistency variance between Guchen oilfield and Xinzhuang oilfield of Biyang sag;

Guidance & evaluation function of gas logging data in Miyang sag viscous crude well drilling;

Geophysical feature of special low-positional geo logic bodies in minor faulted lake basin: case of Miyang sag.;

Technical problems in 3D continuous coverage processing in Miyang Sag;