Crustal structures of blocks with different features associated with tectonic evolution process are got by processing of DSS data of different blocks within the North China rift depression basin.

Lower Paleozoic hydrocarbon-generation history in the mid-south of North China Basin;

Geological interpretation of seismic sections and tectonic evolution of the North China basin;

This paper simulates the mechanism and process of the formation of the ring-like "Large North China Basin" by McKenzie s pure-shear model.

The law of basement pre-existing fabric controlling fault formation and evolution in rift basin

The meso Tethys was formed and extended during the Late Triasso Jurassic,when in the Nyalam area of southern Tibet there were extensive and corresponding sediments accummulated in the rift basin,as well as numerous extension unconformities.

The Mesozoic-Cenozoic extensional tectonic system in eastern China is composed of rift basins and extensional mountain system.

The coupling relationship between basin and mountains is a frontier hot topic for geoscience today, and it is generally considered that fracture systems serves as the coupling links among tectonic groups, such as between extensional orogenic belts and rifting basins, between compressional orogenic belts and foreland basins, as well as between orogenic belts and strike-slip basins.

Potential of the Deep Oil-Gas Reservior-Forming and Direction of the Deep Oil-Gas Exploitation in Southern North China Basin

Overthrust structure on the northern edge of East Qinling - Dabie orogenic belt consists of the southern and the northern overthrust faults, which constitutes the structural link between the East Qinling - Dabie orogenic belt and the southern North China basin.

The Fuyang region,located in the eastern part of the Zhoukou Depression of the southern North China Basin,covers 11000km2,one third of the depression in area.