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Table 2 Rupture models of the Kumamoto earthquake (Asano and Iwata 2016)

From: Stress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, Japan

  Length (km) Width (km) Strike (°) Dip (°)
The northern segment of the mainshock 28 18 235 65
The southern segment of the mainshock 14 18 205 72
The largest foreshock 14 13 212 89