Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

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

The scaling law for slow earthquakes, which is a linear relationship between seismic
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …

Three decades of geodetic monitoring have established slow slip events (SSEs) as a
common mode of fault slip, sometimes linked with earthquake swarms and in a few cases …

Various slow earthquakes (SEQs), including tremors, very low frequency events, and slow
slip events (SSEs), occur along megathrust zones. In a shallow plate boundary region …

A major debate in geophysics is whether earthquakes and slow‐slip events (SSEs) arise
from similar failure mechanisms. Recent observations from different subduction zones …

In shallow subduction zones, fluid behavior impacts various geodynamic processes capable
of regulating slip behaviors and forming mud volcanoes. However, evidence of structures …

Using global navigation satellite system (GNSS) data to detect millimeter-order signals of
short-term slow slip events (S-SSEs) and to estimate their source parameters, especially …

We employ an enhanced data set of Global Positioning System (GPS) velocities to reassess
the slip deficit along the plate interface of the Alaska‐Aleutian subduction zone. An …

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 …