Fig. 11From: 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, JapanSchematic illustration of temporal variations in the depositional systems in which the packets of thick- to very thick-bedded sandstones in the upper Umegase, Kokumoto, and Chonan formations developedBack to article page