Two phases of aseismic afterslip following the March 2021 Damasi, Greece, normal faulting earthquakes retrieved from InSAR measurements. [PDF]
Tolomei C +5 more
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Integrated geophysical, geological, and machine learning approach for structural characterization of the Balakot-Bagh fault zone associated with the 2005 Mw 7.6 Kashmir earthquake. [PDF]
Noor S +5 more
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Tracing the relationship between the upper plate earthquake cycle and megathrust slip, the Atacama fault system in Northern Chile. [PDF]
Gonzalez G +4 more
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Deceleration-phase restrengthening in compositionally zoned fault materials under transient slip. [PDF]
Woo S, Cheon Y, Han R, Lee H, Son M.
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Paleoseismic activity in the moon's Taurus-Littrow valley inferred from boulder falls and landslides. [PDF]
Watters TR, Schmerr NC.
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From foreshock to mainshock: transient sliding velocity sets nucleation time
Fryer B +3 more
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Coseismic crustal seismic velocity changes associated with the 2024 Mw 7.5 Noto earthquake, Japan
Paris N +11 more
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AbstractThe slip budget at a subduction zone megathrust is met by a spectrum of slip behaviors including coseismic slip from great earthquakes, afterslip, episodic tremor and slip (ETS), long‐term slow slip events (SSEs), and quasisteady interseismic creep.
Elizabeth Sherrill, Kaj Johnson
exaly +4 more sources
Fracture energy and breakdown work scaling with coseismic slip
2023Geological observations reveal that earthquakes nucleate, propagate, and arrest in complex fault zones whose structural heterogeneity depends on the tectonic loading, geometry, lithology, rheology, presence of fluids, and strain localization processes. These fault zones can host a wide range of fault slip behaviors (e.g., creep, aseismic- and slow-slip
Elisa Tinti +7 more
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Coseismic Slip Gradient and Rupture Jumps on Parallel Strike‐Slip Faults
Bulletin of the Seismological Society of America, 2015Abstract Field observations of slip distribution along large strike‐slip faults and preliminary rupture model simulations reveal a possible correlation between slip gradient near a fault end and the ability of a rupture to jump over a structure stepover in a strike‐slip fault system.
Zaifeng Liu, Benchun Duan
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