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Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

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. 6

a Downflow (= northeastward) variations in thickness and lithofacies features of thick- to very thick-bedded sandstones in PC4 of the Chonan Formation, Heizo, Ichihara City. b Outcrop photograph of PC4 of the Chonan Formation. A–F denote the locations of the measured sections (A–F) in a. Arrows 1-a and 1-b, and arrows 2-a and 2-b indicate downflow thickening and thinning of sandstone beds in the northeast, respectively. This outcrop (35° 21′ 01″ N, 140° 12′ 10″ E) is located about 400 m east of the location of section 6 in Fig. 5

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