Fig. 5From: Measuring seismicity diversity and anomalies using point process models: case studies before and after the 2016 Kumamoto earthquakes in Kyushu, JapanETAS model fitted to the foreshock sequence. ETAS model (1) is applied to the aftershock sequence of the M6.5 earthquake prior to the occurrence of the M7.3 mainshock, plotted against the ordinary and transformed times via the theoretical cumulative curve of the ETAS model. The red theoretical cumulative curves are superimposed on the black empirical cumulative curves of the aftershocks of M ≥ 1.5, M ≥ 2.0, and M ≥ 2.5 together with the corresponding M–T diagramsBack to article page