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Swiss Journal of Geosciences
Fig. 12 | Swiss Journal of Geosciences

Fig. 12

From: Sedimentary architecture of shallow-water fan-delta front in a lacustrine basin: Sangyuan section of Lower Cretaceous Xiguayuan Formation, Luanping Basin, northeast China

Fig. 12

Vertical grain-size trend of mouth bar accretions varies with grain size. Accretions involving coarse-grained sediments (median grain size is > 1000 μm) display fining-upward trends, whereas those with fine-grained sediments (< 1000 μm) are characterized by inverse grading

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