Figure 8
From: Kibi Plateau: A stable-coherent tectonic unit in the active Japanese Islands
(a) Photo of the outcrop of Paleogene shallow marine sediments without any significant inclination observed in the small island (Maejima) of Seto Inland Sea. The sediments consist mainly of sandstone and conglomerates containing the fossils of Molluscan fauna22 and Scalpellid-dominated barnacle assemblages23, and trace fossils21. The rectangular box shows the area of the photo (b). (b) Photo of the rectangular part (b) in photo (a) showing the trace fossils.
