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Progress in Earth and Planetary Science
Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

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. 10

Downflow changes in thickness and lithofacies types of two sandstone beds below the Ku1 tephra key bed. The inset map shows the locations of the measured sections. See Table 1 for descriptions and interpretations of lithofacies types. The trend of this stratigraphic cross-section (74°) is oblique to the paleocurrent directions (47–70°)

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