Fig. 5From: Sedimentary architecture of shallow-water fan-delta front in a lacustrine basin: Sangyuan section of Lower Cretaceous Xiguayuan Formation, Luanping Basin, northeast ChinaSedimentary architecture of type B channel deposits. Lithofacies associations in type B channel deposits are complex, but in general, these involve the C3, C4, and C6 in the bottom, which are overlain by the S1, S2 and S3Back to article page