Abstract
Tectonosedimentary analysis of sedimentary basins mainly includes the study of tectonostratigraphic architectures, structural frameworks, uplift/depression distribution patterns, and syndepositional structures and their control on depositional facies and sediment dispersal systems. It is very important to identify tectonic unconformities and their composite patterns and reconstruct the paleouplift landform based on integrated analysis of seismic and other geological data. The study of syndepositional faults and tectonopaleogeomorphology, especially the structural slope break zone formed by long-term active syndepositional faults, is the key to revealing the structural control on the development and distribution of sedimentary systems or systems tracts.
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