Results 81 to 90 of about 2,530 (204)
Imaging rapid early afterslip of the 2016 Pedernales earthquake, Ecuador
High-Rate (HR) GPS time series following the 2016 Mw 7.8 Pedernales earthquake suggest significant postseismic deformation occurring in the early postseismic period (i.e. first few hours after the earthquake) that is not resolved with daily GPS time series.
Tsang, Louisa L.H. +9 more
openaire +3 more sources
Insights on earthquake triggering processes from early aftershocks of repeating microearthquakes [PDF]
Characterizing the evolution of seismicity rate of early aftershocks can yield important information about earthquake nucleation and triggering. However, this task is challenging because early aftershock seismic signals are obscured by those of the ...
Ampuero, J.-P., Lengliné, O.
core +3 more sources
Investigating the spatial distribution of coseismic rupture, postseismic afterslip, and their interactions is essential for understanding the heterogeneous frictional characteristics of faults, and seismic hazard assessments.
Xinyue Lei +9 more
doaj +1 more source
On February 27th 2010, a MW8.8 earthquake struck the coast of south‐central Chile, rupturing ∼500 km along the subduction interface. Here we estimate the amount of seismically‐released afterslip (SRA) and the mechanisms underlying the distribution of ...
Hans Agurto +3 more
doaj +1 more source
Dual Role of a Subducted Seamount in Megathrust Rupture Initiation and Rupture Barrier
Abstract Using high‐resolution 3D tomography and a relocated 2010–2022 earthquake catalog, we identify a seamount at 20–25 km depth beneath the Mompiche–Cojimíes region in the coastal forearc of Ecuador. This provides a rare, well‐resolved example of seamount preservation at these depths. The seamount coincides with a low interseismic‐coupling corridor
G. Ponce +6 more
wiley +1 more source
Subducted rough topography complicates seismic and aseismic slip behavior. The 2024 M 7.1 Hyuganada earthquake occurred along the megathrust with ridge subduction.
Yuji Itoh
doaj +1 more source
Abstract The Qilian‐Haiyuan fault system is the main tectonic boundary of the northeastern Tibetan Plateau, controlling the regional tectonic deformation and seismic activity. Extensive Sentinel‐1 SAR data (2014–2021) are used to map the regional tectonic deformation, strain distribution, and locking along primary and secondary faults.
Donglin Wu +6 more
wiley +1 more source
This study investigated postseismic deformation resulting from the 2024 Noto Peninsula earthquake on January 1. Particular focus was placed on the displacement observed in Sado Island, which is located several tens of kilometers east of the eastern end ...
Miku Ohtate, Yusaku Ohta, Yuta Mitsui
doaj +1 more source
Detection and Modeling of the Effect of Large Earthquakes in GRACE/GRACE‐FO Mascons
Abstract The usefulness of Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow‐On (GRACE/FO) data products for ocean studies remains limited in a few areas, where large gravity signals from the 2011 Japan earthquake and three major earthquakes in the Andaman‐Sumatra area (in 2004, 2007, and 2012) obscure vastly smaller signals of interest ...
Jennifer A. Bonin +4 more
wiley +1 more source
Reactivated afterslip induced by a large regional earthquake, Fiordland, New Zealand
AbstractThe evaluation of seismic hazard along active faults requires knowledge of the long term slip rate, the portions of the fault which are accumulating strain, and the magnitude, number, and location of past earthquakes. Aseismic slip will lower the long‐term seismic potential, but the distribution of seismic versus aseismic slip along faults is ...
I. J. Hamling, S. Hreinsdóttir
openaire +1 more source

