In the past 30 years, the small baseline subset (SBAS) InSAR time-series technique has
emerged as an essential tool for measuring slow surface displacement and estimating …

The 2011 Tohoku-oki earthquake produced the most well-recorded postseismic deformation
of any megathrust earthquake in the world. Over the last decade, researchers have used a …

This article proposes deep convolutional neural networks to detect and map localized, rapid
subsidence caused by mining activities using time-series Sentinel-1 synthetic aperture radar …

The deformation transient following large subduction zone earthquakes is thought to
originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on …

Understanding the rheological properties of the upper mantle is essential to develop a
consistent model of mantle dynamics and plate tectonics. However, the spatial distribution …

The diverse mechanical behaviors of subduction zones during the seismic cycle emerge
from the nonlinear dynamics of a complex mechanical system with interacting brittle and …

Postseismic deformation following great subduction earthquakes is commonly modeled as
the sum of the contributions from afterslip on the megathrust and viscoelastic relaxation of …

The 2016 Kumamoto earthquake sequence occurred on the Futagawa–Hinagu fault zone
near the Aso volcano on Kyushu island. The sequence was initiated with two major (Mw≥ …

Deformation associated with plate convergence at subduction zones is accommodated by a
complex system involving fault slip and viscoelastic flow. These processes have proven …

Cascade-up and/or slow-slip processes are commonly believed to control interactions
between foreshocks, mainshocks and aftershocks, but their relative contributions remain …