Results 81 to 90 of about 7,906 (216)

Shallow Creep in the Leaky Stress Shadow of Locked Zones of Subduction Megathrust

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract In some subduction zones such as Nankai, creeping of the shallow part of the megathrust in the stress shadow of deeper locked zones is detected by seafloor geodetic measurements and/or reflected by slow earthquakes (SEQs). Here we explain that shallow creep occurs in the stress shadow for two reasons: (a) prolonged afterslip and (b) a leaky ...
Kelin Wang, Yajing Liu, Tianhaozhe Sun
wiley   +1 more source

Linking 3D Long‐Term Slow‐Slip Cycle Models With Rupture Dynamics: The Nucleation of the 2014 Mw 7.3 Guerrero, Mexico Earthquake

open access: yesAGU Advances
Slow slip events (SSEs) have been observed in spatial and temporal proximity to megathrust earthquakes in various subduction zones, including the 2014 Mw 7.3 Guerrero, Mexico earthquake which was preceded by a Mw 7.6 SSE.
Duo Li, Alice‐Agnes Gabriel
doaj   +1 more source

Fast, accurate solutions for curvilinear earthquake faults and anelastic strain [PDF]

open access: yes, 2018
Imaging the anelastic deformation within the crust and lithosphere using surface geophysical data remains a significant challenge in part due to the wide range of physical processes operating at different depths and to various levels of localization that
Barbot, Sylvain, Landry, Walter
core   +1 more source

A secondary zone of uplift due to megathrust earthquakes [PDF]

open access: yesPure and Applied Geophysics, 2019
ISSN:0033 ...
van Dinther, Ylona   +2 more
openaire   +5 more sources

Hydraulic Control of the Foreshocks and Mainshock of the 2017 Valparaíso, Chile, Earthquake

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract Slow‐slip events (SSE) are a key mode of aseismic deformation and can enhance fault permeability through fracturing, enabling fluid migration from the overpressured oceanic crust to the plate interface. Whether the resulting poroelastic stress changes promote seismicity and larger megathrust events, however, remains unclear.
Carlos Peña   +4 more
wiley   +1 more source

Ground Shaking and Seismic Source Spectra for Large Earthquakes around the Megathrust Fault Offshore of Northeastern Honshu, Japan [PDF]

open access: yes, 2013
Large earthquake ruptures on or near the plate boundary megathrust fault offshore of northeastern Honshu, Japan, produce variable levels of regional high‐frequency ground shaking.
Kanamori, Hiroo   +2 more
core   +1 more source

Cascadia megathrust rupture model

open access: yes, 2020
Data products of Cascadia megathrust rupture ...
openaire   +1 more source

Relationship between citizens' risk perceptions formed by disaster information and migration decision-making: Evidence from Japan

open access: yesProgress in Disaster Science, 2020
This study approached the problem of how disaster-related information from various media leads to citizens recognizing risk, and how this affects migration decision-making.
Ryohei Yamashita
doaj   +1 more source

Stress Transfer From Slow Slip Events to Earthquake Swarms as a Cycle in the Southernmost Ryukyu Subduction Zone

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract Recent megathrust earthquakes preceded by slow slip events highlight static stress transfer as a key triggering mechanism. However, there are limited insights into the interplay between static stress transfer and elevated fluid pressure before earthquake triggering.
Sean Kuanhsiang Chen   +4 more
wiley   +1 more source

Impact of a tsunami generated at the Lesser Antilles subduction zone on the Northern Atlantic Ocean coastlines [PDF]

open access: yesAdvances in Geosciences, 2014
On 11 March 2011, a Mw ~ 9.0 megathrust earthquake occurred off the coast of Tohoku, triggering a catastrophic tsunami reaching heights of 10 m and more in some places and resulting in lots of casualties and destructions.
J. Roger, A. Frère, H. Hébert
doaj   +1 more source

Home - About - Disclaimer - Privacy