A seismic geomorphology study of the fluvial and lacustrine-delta facies of the Cretaceous Quantou-Nenjiang Formations in Songliao Basin, China
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文摘

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.

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