Results 71 to 80 of about 748 (174)
Abstract Forward and inverse modeling techniques are often applied to paleotsunamis to reconstruct inundation parameters. The accuracy of both types of models can be influenced by geomorphology, particularly in areas such as northern Cascadia, where rocky headlands and fjords influence tsunami flow and the preservation of sedimentary deposits ...
Stephen E. Bartlett +11 more
wiley +1 more source
Interseismic Creep Along the Enriquillo–Plantain Garden Fault, Haiti, Estimated From InSAR
Abstract The Enriquillo–Plantain Garden fault zone (EPGFZ) is a major left‐lateral strike‐slip fault in southern Haiti hosting several recent destructive earthquakes, including the 2021 MW 7.1 Nippes event with primary thrust‐slip. To investigate how strain is accommodated in the vicinity of the 2021 event, we analyzed Sentinel‐1 interferometric ...
Rishabh Dutta +2 more
wiley +1 more source
Fast report: near-real-time assessment of the ML6.4 Dapu earthquake-induced landslides
Rapid assessment of potential landslides in regions of risk and their associated impacts following an earthquake is needed to provide crucial information to guide emergency responses.
Kai-Shyr Wang +4 more
doaj +1 more source
Coseismic gravity and displacement changes of Japan Tohoku earthquake (Mw 9.0)
AbstractThe greatest earthquake in the modern history of Japan and probably the fourth greatest in the last 100 years in the world occurred on March 11, 2011 off the Pacific coast of Tohoku. Large tsunami and ground motions caused severe damage in wide areas, particularly many towns along the Pacific coast. So far, gravity change caused by such a great
Xinlin Zhang +3 more
openaire +2 more sources
Abstract This study investigates whether hydraulic fracturing contributed to the 2021 Ms 6.0 Luxian earthquake in the Sichuan Basin. Time‐series InSAR analysis of multi‐temporal Sentinel‐1 data reveals coseismic deformation associated with the 2021 Luxian earthquake and localized uplift near hydraulic fracturing platforms.
Xiaoran Fan +3 more
wiley +1 more source
On August 18, 2020, an MW 6.8 earthquake occurred ~130 km southwest of Bengkulu. In this study, we used the static GNSS data from continuously monitoring stations, surrounding the epicentre, to obtain the data from 10 days before to 10 days after the ...
O. Anggara +3 more
doaj +1 more source
Abstract Constraining peak temperature during seismic slip is essential for quantifying earthquake energy budgets and fault weakening. Rock magnetic methods provide a sensitive means of estimating shear‐induced coseismic temperature rise; however, the role of fluids in friction‐induced magnetic alterations remains poorly constrained.
Qiang Fu +6 more
wiley +1 more source
The strongest earthquakes with magnitudes Mw 8–9 generate coseismic displacements of the Earth’s crust, covering entire regions of the world. These displacements can be recorded using observations provided by the independent geodetic GNSS networks.
N. V. Shestakov +8 more
doaj +1 more source
A probabilistic model for coseismic vertical displacement hazard in coastal settings
Characterizing coastal multi-hazards in tectonically active regions requires considering possible coseismic vertical deformation. Coseismic uplift or subsidence can cause near-instantaneous meter-scale relative sea level changes that can exacerbate or reverse the effects of ongoing global sea-level rise.
Jaime Delano +6 more
openaire +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

