Episodes and geodynamic setting of Himalayan movement in China;

Himalayan movement originated from powerful compressive stress in Tethys tectonic domain, which caused north Tianshan mountains to quick and extensive uplift and thrusting toward Junggar basin followed by shaping foreland depression of intracontinental orogenic type developed in the southern margin of Junggar basin.

Himalayan movement in this basin can be divided into eleven stages in terms of weak-strong intensity of structural compression.

Himalayan tectonic movement has significant influence on the geology evolution and the oil-gas reservoir formation in the Ordos Basin.

Himalayan tectonic movement plays important role in the Cenozoic tectonic pattern of the west China.

Characteristics and petroleum geological significance of Himalayan orogeny in Kuqa foreland basin;

Expression of the Himalayan orogeny in the Kuqa depression, Tarim basin——evidence from the rock acoustic emission experiment;

Himalayan orogeny refers to the tectonic movement from Cenozoic, and it is the main power responsible for the formation of depressions and traps.

The results indicate that a huge amount of crustal shortening took place in a nearly N-S direction in the central part of Qinghai-Tibet Plateau in the late Himalayan age, with the average shortening amount reaching 30% , while a huge amount of c.

The characteristics of intra-continental deformation and hydrocarbon distribution controlled by the Himalayan tectonic movements in China;