Based on the logical consequence and the characters of possible development of basin,two ideal styles of depositional response in basin are proposed for the first time.

Mesozoic tectonic events in Ordos Basin and their sedimentary responses;

For the first time,the authors have systematically studied the sedimentary response to Triassic-Jurassic thrust faulting in the foreland thrust belt of northwestern Junggar Basin by using the theory and method of tectono-sedimentology and foreland basin analysis.

For the first time, the authors systemically studied sedimentary response to the activity of the Permian thrust faulting in the foreland thrust belt of the northwestern Junggar basin in based on the theory and method of tectono-sedimentology and foreland basin analyses.

Two kinds of slope-breaks are developed in this basin, one is the syndepositional fault slope-break, the other is the syndepositional bend slope-break, whic.

The controls of the syndepositional faults are manifested in:(1) the controls of the active basin-margin faults in the steep slope zone on the distribution of the fan delta facies;(2) the controls of the active basin-margin faults in the ramp zone on the distribution of the braided delta facies;(3) the c.

The study proved that horizontal migration of platform margin was mainly controlled by syndepositional faults,the vertical sequence evolution of platform margin was mainly controlled by sea-level change,the type of margin reef-bank was controlled by different types of carbonate secret organisms.

The petrological and petrochemical characteristics indicate that the formation of these conglomerates was controlled by synsedimentary faults during the metallogenic e.