Fig. 12From: Deep crustal structure around the Atotsugawa fault system, central Japan: A weak zone below the seismogenic zone and its role in earthquake generationSchematic interpretation of velocity heterogeneity along the Atotsugawa fault. Gray and white circles denote small earthquakes and low-frequency earthquakes, respectively. The estimated fluid fraction (ø) are shown for pyroxene amphibolite and for hornblende-pyroxene gabbro (in parentheses). Note that volume fractions of aqueous fluids for the horizontally isolated low-velocity zone in the upper crust beneath the central section are estimated to be 0.2–0.3%.Back to article page