Fig. 7
From: Non-stationary ETAS to model earthquake occurrences affected by episodic aseismic transients
Results for the GeoNet catalog analyzed using non-stationary ETAS model. The magnitudes of earthquakes in the catalog examined in the study are plotted versus time in (a). The computed L-curve along with the point corresponding to the chosen smoothness parameter is shown in (b). The background rate functions estimated using the models NS_L_MP and NS_Adapt are presented in (c, d) respectively, along with the error bounds computed using Hessian matrix of \(\Phi\) at the solution