Results 141 to 150 of about 1,060 (180)

Coseismic deformation analysis of the 2017 Milin Ms 6.9 earthquake in the Namche Barwa Syntaxis: Implications for regional tectonics. [PDF]

Fundam Res
Wang J, Zhang S, Zhao Y, Cai F, Wang C, He J, Ding L.   +6 more
europepmc   +1 more source

Frictional healing and induced earthquakes on conventionally stable faults. [PDF]

Nat Commun
Li M, Niemeijer AR, van Dinther Y.
europepmc   +1 more source

Influence of different factors on coseismic deformation of the 2015 Mw7.8 earthquake in Nepal. [PDF]

Sci Rep
Wu R, Dong X, Xia B, Wang W, She X, Chu Z.   +5 more
europepmc   +1 more source

From foreshock to mainshock: transient sliding velocity sets nucleation time

Fryer B, Garagash D, Lebihain M, Passelègue F.   +3 more
europepmc   +1 more source

Coseismic crustal seismic velocity changes associated with the 2024 Mw 7.5 Noto earthquake, Japan

Paris N, Itoh Y, Brenguier F, Wang Q, Sheng Y, Okada T, Uchida N, Higueret Q, Takagi R, Sakai S, Hirahara S, Kimura S.   +11 more
europepmc   +1 more source

Coseismic slip distribution of the 1923 Kanto earthquake, Japan [PDF]

Journal of Geophysical Research, 2005
The slip distribution associated with the 1923 M = 7.9 Kanto, Japan, earthquake is reexamined in light of new data and modeling. We utilize a combination of first‐order triangulation, second‐order triangulation, and leveling data in order to constrain the coseismic deformation.
Takuya Nishimura, Fred Pollitz
exaly   +2 more sources

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New Insights Into the Slip Budget at Nankai: An Iterative Approach to Estimate Coseismic Slip and Afterslip

Journal of Geophysical Research: Solid Earth, 2021
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

2023
Geological 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, Massimo Cocco, Stefano Aretusini, Chiara Cornelio, Stefan B. Nielsen, Elena Spagnuolo, Paul Selvadurai, Giulio Di Toro   +7 more
openaire   +1 more source

Coseismic Slip Gradient and Rupture Jumps on Parallel Strike‐Slip Faults

Bulletin of the Seismological Society of America, 2015
Abstract 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
openaire   +1 more source