S Dhar, J Muto, Y Ohta, T Iinuma - Progress in Earth and Planetary Science, 2023 - Springer
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 …
Z Wu, T Wang, Y Wang, R Wang… - IEEE Transactions on …, 2021 - ieeexplore.ieee.org
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 …
S Barbot - Earth, Planets and Space, 2020 - Springer
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 …
J Fukuda, KM Johnson - Journal of Geophysical Research …, 2021 - Wiley Online Library
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 …
H Yue, J Sun, M Wang, Z Shen, M Li, L Xue… - Earth and Planetary …, 2021 - Elsevier
Cascade-up and/or slow-slip processes are commonly believed to control interactions between foreshocks, mainshocks and aftershocks, but their relative contributions remain …