Seismicity usually exhibits a non‐Poisson spatiotemporal distribution and could undergo nonstationary processes. However, the Poisson assumption is still deeply rooted in current …
The distribution of earthquakes in time and space is seldom stationary, which could hinder a robust statistical analysis, particularly in low‐seismicity regions with limited data. This work …
Probabilistic seismic hazard analysis requires a seismicity rate model, or in other words, a forecast of earthquake rates. In the New Zealand National Seismic Hazard Model 2022, the …
Historical and instrumental earthquake catalogs in low strain rate regions are not necessarily indicative of the long-term spatio-temporal distribution of seismicity. This implies …