Fig. 5From: Volcanic magma reservoir imaged as a low-density body beneath Aso volcano that terminated the 2016 Kumamoto earthquake ruptureCalculated density contrast model projected onto Fault B. Fault B makes up one-sixth of the NE side of the total fault model created by using InSAR observations of ground deformation of the 2016 Kumamoto earthquake (Geospatial Information Authority of Japan 2016b). No aftershocks occurred in the first 3 days after the mainshock within 3 km of the plane of Fault B (Fig. 1b). Density distributions are plotted using linear interpolationBack to article page