A geological model of point bar is established and the method to identify paleocurrent direction is proposed.
Two types of delta were recognized in Yaojia Formation of Songliao Basin.
Large-scale turbidity current systems have been found in the TST of k2n1 Formation.
Fourteen sub-lacustrine fans in different sizes were formed by turbidity current flowing from the delta to the lake.
The sedimentary model provides a guiding significance and a new technological means for the optimization of exploration targets.