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The right-slip Talas-Ferganhna fault plays significant roles in controlling the strata, structures and petroleum geologic features in Kashi sag since Late Triassic. During the Late Triassic-Middle Jurassic, Kuzgongsu and Kezletao fault basins probably disconnected with each other occurred in the sag, with developed rifted-style source rocks of Lower-Middle Jurassic. During the Neogene-Quaternary, the relevant strike-slip deformation of the fault occurred and controlled the petroleum traps and accumulations in Kashi sag.
The right-slip Talas-Ferganhna fault plays significant roles in controlling the strata, structures and petroleum geologic features in Kashi sag since Late Triassic. During the Late Triassic-Middle Jurassic, Kuzgongsu and Kezletao fault basins probably disconnected with each other in the sag , along the Neogene-Quaternary, the relevant strike-slip deformation of the fault occurred and controlled the petroleum traps and accumulations in Kashi sag.