Results 131 to 140 of about 319 (157)

Seismic energy from small earthquakes maps fault segmentation in the Southeastern Alps. [PDF]

open access: yesSci Rep
Picozzi M   +11 more
europepmc   +1 more source

Earthquake swarms and slow slip on a sliver fault in the Mexican subduction zone. [PDF]

open access: yesProc Natl Acad Sci U S A, 2019
Fasola SL   +4 more
europepmc   +1 more source

Intrinsic factors responsible for brittle versus ductile nature of refractory high-entropy alloys. [PDF]

open access: yesNat Commun
Tsuru T   +9 more
europepmc   +1 more source

Evidence of megathrust earthquakes and seismic supercycles in subtropical Japan from millennia-old coral microatolls. [PDF]

open access: yesNat Commun
Debaecker S   +12 more
europepmc   +1 more source

Afterslip, Tremor, and the Denali Fault Earthquake

Bulletin of the Seismological Society of America, 2012
We tested the hypothesis that afterslip should be accompanied by tremor using observations of seismic and aseismic deformation surrounding the 2002 M  7.9 Denali fault, Alaska, earthquake (DFE). Afterslip happens more frequently than spontaneous slow slip and has been observed in a wider range of tectonic environments, and thus the existence or absence
J. Gomberg, S. Prejean, N. Ruppert
openaire   +1 more source

On the mechanics of earthquake afterslip

Journal of Geophysical Research: Solid Earth, 1991
We propose a model for earthquake afterslip based on rate and state variable friction laws. In the model, afterslip is attributed to the interaction of a velocity‐weakening region at depth (within which earthquakes nucleate) with an upper region of velocity‐strengthening frictional behavior.
Marone C. J., Scholtz C. H., Bilham R.
openaire   +2 more sources

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