Fig. 10From: Measuring seismicity diversity and anomalies using point process models: case studies before and after the 2016 Kumamoto earthquakes in Kyushu, JapanEarthquake detection-rate parameters and b-value estimates. The panels show, from top to bottom, the b-value time change and the detection-rate parameters with double error (95%) envelopes versus time on a logarithmic scale. The vertical dashed lines show the occurrence times of the M6.4 and M7.3 earthquakes, which are marked by large circlesBack to article page