Fig. 9From: Postseismic fluid discharge chemically recorded in altered pseudotachylyte discovered from an ancient megasplay fault: an example from the Nobeoka Thrust in the Shimanto accretionary complex, SW JapanComparing with Cf0 value and modern pore fluids sampled from various settings. Vertical axis shows Cf0 values. Green, blue, and red diamond shows Cf0 values at temperatures of 250, 300, and 350 °C, respectively. Four black lines show concentrations of interstitial fluid at Mid-Atlantic Ridge (Campbell et al. 1988), Juan de Fuca Ridge (Butterfield et al. 1994), Escanaba Trough (Campbell et al. 1994), and Nankai Trough (Nishio et al. 2015), respectivelyBack to article page