Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Earthquakes can change the stress field in the Earth's lithosphere as they relieve and
redistribute stress. Earthquake‐induced stress changes have been observed as temporal …

The earthquake magnitude‐frequency distribution is characterized by the b‐value, which
describes the relative frequency of large versus small earthquakes. It has been suggested …

Abstract We, the ongoing Working Group on California Earthquake Probabilities, present a
spatiotemporal clustering model for the Third Uniform California Earthquake Rupture …

Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

Probabilistic forecasting of earthquake‐producing fault ruptures informs all major decisions
aimed at reducing seismic risk and improving earthquake resilience. Earthquake forecasting …

Megathrust earthquakes release and transfer stress that has accumulated over hundreds of
years, leading to large aftershocks that can be highly destructive. Understanding the …

Knowledge of the state of stress in subducting slabs is essential for understanding their
mechanical behavior and the physical processes that generate earthquakes. Here, we …

Numerous normal‐faulting aftershocks in subduction forearcs commonly follow large
megathrust earthquakes. Postseismic normal faulting has been explained by stress changes …

Along the margins of orogenic plateaus, the viscous Earth structure and fault geometries
play a primary role in controlling the tectonic evolution and earthquake generation. After the …