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Fig. 9 | Progress in Earth and Planetary Science

Fig. 9

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. 9

Downflow changes in lithofacies types of sandstone beds above the Ku1 tephra key bed in PK2 of the Kokumoto Formation along the Yoro River (Location 4 in Fig. 4). The inset map shows the locations of the measured sections. See Table 1 for descriptions and interpretations of lithofacies types

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