Fig. 2From: Measuring seismicity diversity and anomalies using point process models: case studies before and after the 2016 Kumamoto earthquakes in Kyushu, JapanThe ETAS model fitted to the seismicity in the subregions prior to the Kumamoto earthquakes. a The total area of Fig. 1a is divided into subregions R1–R8. The thin rectangles indicate the fault models (Geospatial Information Authority of Japan 2016). b The ETAS estimate of the cumulative curve (red curve) is superimposed on the observed cumulative curve (black curve) in ordinary time (the left side of each pair) and transformed time (the right side of each pair). The corresponding M–T plots are attached at the bottom of each panelBack to article page