Fault-zone fluids control effective normal stress and fault strength. While most earthquake
models assume a fixed pore fluid pressure distribution, geologists have documented fault …

Earthquakes are caused by the release of tectonic strain accumulated between events.
Recent advances in satellite geodesy mean we can now measure this interseismic strain …

Dynamic modeling of sequences of earthquakes and aseismic slip (SEAS) provides a self‐
consistent, physics‐based framework to connect, interpret, and predict diverse geophysical …

Numerical simulations of sequences of earthquakes and aseismic slip (SEAS) have made
great progress over past decades to address important questions in earthquake physics …

Mature strike‐slip faults are usually surrounded by a narrow zone of damaged rocks
characterized by low seismic wave velocities. Observations of earthquakes along such faults …

As concerns rise over damaging earthquakes related to industrial activities such as
hydraulic fracturing, geothermal energy extraction and wastewater disposal, it is essential to …

It is widely recognized that fluid injection can trigger aseismic fault slip. However, the
processes by which the fluid‐rock interactions facilitate or inhibit slip are poorly understood …

There is a growing recognition that subsurface fluid injection can produce not only
earthquakes, but also aseismic slip on faults. A major challenge in understanding …

This study addresses the stress–strain relaxation functions of solid polymers in the
framework of the linear viscoelasticity with aim to establish the adequate fractional operators …

Abstract The Nankai Trough in Southwest Japan exhibits a wide spectrum of fault slip, with
long-term and short-term slow-slip events, slow and fast earthquakes, all associated with …