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Fig. 8 | Progress in Earth and Planetary Science

Fig. 8

From: Spatial and temporal variations in depositional systems in the Kazusa Group: insights into the origins of deep-water massive sandstones in a Pleistocene forearc basin on the Boso Peninsula, Japan

Fig. 8

Downflow changes in thickness, lithofacies types, and grain sizes of a sandstone bed developed just above the U2 tephra key bed in the Umegase Formation. The inset map shows the locations of the measured sections. Black filled circles in grain-size diagrams denote volume percentages of muddy grains less than 20 μm. See Table 1 for descriptions and interpretations of lithofacies types

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