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Fig. 5 | Earth, Planets and Space

Fig. 5

From: New hypothesis to explain Quaternary forearc deformation and the variety of plate boundary earthquakes along the Suruga–Nankai Trough by oblique subduction of undulations on the Philippine Sea Plate

Fig. 5

Vertical movement along the southern coast of the Kii Mountains. a Location of survey sites shown by small squares with symbols and coseismic vertical movements during the 1944 and 1946 Showa earthquakes by black solid lines in meter. b Height distribution of the MIS 5e terrace (Yonekura 1968). Symbols at the bottom indicate locations shown in a. c Height distribution of emergent fossil assemblages. Symbols at the bottom indicate locations shown in a (revised from Shishikura et al. 2008). d Photo of a vertical slice from fossil assemblage shown in c. Red circles are positions of 14C age samples. White dotted lines indicate discontinuous boundaries

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