Tsunamigenic fault structures revealed in the 2024 Noto earthquake (M7.6) rupture area. [PDF]
Park JO +8 more
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Ce travail de thèse a pour but d'analyser les variations de vitesses sur des grandes failles décrochantes en contexte intracontinental, capables de produire des séismes de très fortes magnitudes (M > 7.5). Afin d'illustrer ces variations d'activités, cette analyse a été effectuée sur deux zones d'études situées en domaine continental et sismiquement ...
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InSAR analysis reveals insights into the Ms 6.2 earthquake rupture and tectonic dynamics of the northeast margin of the Qinghai‒Tibet plateau. [PDF]
Sun G, Guo F, Guo X, Li M, Peng B.
europepmc +1 more source
Dynamic restrengthening and fault heterogeneity explain megathrust earthquake complexity. [PDF]
Wong JWC, Gabriel AA, Fan W.
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Stress-mediated multi-fault rupture dynamics of the 2023 Kahramanmaraş earthquake sequence, Türkiye. [PDF]
Nalbant SS +4 more
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Deciphering stress perturbations throughout the 2025 M<sub>w</sub> 7.1 Dingri, Southern Xizang Earthquake. [PDF]
Ma Z +8 more
europepmc +1 more source
Analyzing Fault Reactivation Behavior Using InSAR, Stress Inversion, and Field Observations During the 2025 Sındırgı Earthquake Sequence, Simav Fault Zone, Western Türkiye. [PDF]
Kutoğlu ŞH +4 more
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Coseismic slip and afterslip of the 2024 Hyuganada earthquake modulated by subducted seamount
Subducted rough topography complicates seismic and aseismic slip behavior. The 2024 M 7.1 Hyuganada earthquake occurred along the megathrust with ridge subduction. We inferred coseismic slip and afterslip using geodetic displacements to observationally illustrate the role of subducted seamounts in modulating seismic and aseismic slip processes.
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Interplate rheological contrast revealed by asymmetric deformation after the 2023 Kahramanmaraş earthquakes. [PDF]
Liu J +4 more
europepmc +1 more source

