Results 71 to 80 of about 1,060 (180)
Coseismic Shallow Slip Deficit Accounted for by Diffuse Off‐Fault Deformation
AbstractEarthquake ruptures produce fault slip and kilometer‐wide diffuse deformation of the host rocks. However, the origin of the diffuse deformation and its role in the rupture process are debated. We produce a refined slip model for the 2019 Ridgecrest, California, earthquakes, and analyze the relations between down‐dip rupture process, and surface
Solene Antoine +3 more
openaire +3 more sources
The main objective of this work is to determine whether is it possible to use the Phase Variation Methodology in an early warning context. For this, it is sought to determine the value of alpha that best reproduces the inundation observed for the Maule event (2010), and that is capable of reproducing the uncertainty that a tsunami prediction process ...
Amanda Cabrera, Patricio Catalan
openaire +2 more sources
Coseismic and Postseismic Deformations of the 2023 Turkey Earthquake Doublet
On 6 February 2023, an earthquake doublet of Mw 7.8 and Mw 7.5 occurred in southeastern Turkey and caused surface ruptures over 350 km for the eastern Anatolian fault (EAF) and 150 km for the Surgu fault (SF), respectively. Over 3700 Mw > 3.0 aftershocks
Chaoya Liu +4 more
doaj +1 more source
Abstract The Hellenic subduction system is the primary locus of Nubia‐Eurasia convergence, yet the distribution of strain accumulation along it is still debated. Here, we invert 832 geodetic velocities and 146 earthquake slip vectors to assess the spatial variability of interseismic locking and provide new constraints on the rate of slip deficit ...
Konstantinos Chousianitis +4 more
wiley +1 more source
Brittle Creep as a Mechanism for Postseismic Relaxation in Upper Crustal Dolomite Marble
Abstract In many locations, earthquakes in the upper crust occur in carbonate rocks, whose deformation affects aftershock sequences and postseismic relaxation. We investigate the stress relaxation process and strain evolution in Jinping dolomite marble (porosity <0.2%) subjected to multi‐stage stress ramp‐relaxation cycles under confining pressures of ...
Shuting Miao +4 more
wiley +1 more source
Temperature Dependence of Fault Frictional Healing in Quartz Gouges at Hydrothermal Conditions
Abstract Fault healing allows the accumulation of stress along faults during interseismic periods. In this critical stage, temperature‐dependent fluid‐rock interactions within fault zones become crucial at seismogenic depth in controlling fault strength recovery. However, frictional healing at hydrothermal conditions is still underexplored.
G. Guglielmi, G. Di Toro, T. Tesei
wiley +1 more source
Towards Linking Coseismic Slip to Interseismic Coupling at Cascadia
Final report for a project funded by the Cascadia Region Earthquake Science Center (CRESCENT) Seed Grant Program (2024-25).
Johnson, Kaj, Sherrill, Elizabeth
openaire +2 more sources
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
The coseismic deformation field on both sides of the fault, especially the distribution and change characteristics of near-field deformation, not only provides important constraints for the fine inversion of the slip distribution model but also serves as
Yujing Song +6 more
doaj +1 more source
On August 8, 2017, the Jiuzhaigou Mw 6.5 earthquake occurred in Sichuan province, southwestern China, along the eastern margin of the Tibetan Plateau. The epicenter is surrounded by the Minjiang, Huya, and Tazang Faults.
Zhaosheng Nie +4 more
doaj +1 more source

