Fig. 9From: Measuring seismicity diversity and anomalies using point process models: case studies before and after the 2016 Kumamoto earthquakes in Kyushu, JapanNon-stationary ETAS model and model (2) applied to the Oita subregion (S3 in Fig. 6a). The marks, line types, and colors are the same as indicated in Fig. 7, except that the thick green curve represents the triggering effect of the M7.3 mainshock indicated by the third term in model (2)Back to article page