Figure 5From: Mechanism of long-standing Cenozoic basin formation in central Hokkaido: an integrated basin study on an oblique convergent margin An E-W seismic profile crossing transcurrent faults on the northeast Japan forearc region. Data were acquired in a MITI survey (JNOC 1974). See Figure 1 for line location. Geologic interpretation is after Takano et al. (2013).Back to article page