Fig. 5From: Seismotectonics of the 2018 northern Osaka M6.1 earthquake and its aftershocks: joint movements on strike-slip and reverse faults in inland JapanAssessment of the uncertainty of the major and minor DC MTs decomposed from the whole posterior ensemble of 10,000 solutions (see text). a Perturbed nodal planes of the DC beach-ball in lower hemisphere projection. b Histogram of their mutual scalar seismic moment ratio. The triangle diagram (Frohlich 1992) with perturbed solutions in (c) indicates the uncertainty of the faulting typeBack to article page