Fig. 13From: Characteristics of secondary-ruptured faults in the Aso Caldera triggered by the 2016 Mw 7.0 Kumamoto earthquakeResults of the synthetic test. a Estimated width of the fault as a function of the actual width. Solid line shows the relation of estimated width equals the actual width. One can convert to the bottom depth by dividing the values by \(\sqrt{2}\). b Estimated dip of the fault as a function of the actual width. Solid line shows the actual dip of 45°Back to article page