Seismic energy from small earthquakes maps fault segmentation in the Southeastern Alps. [PDF]
Picozzi M +11 more
europepmc +1 more source
Earthquake swarms and slow slip on a sliver fault in the Mexican subduction zone. [PDF]
Fasola SL +4 more
europepmc +1 more source
Machine learning predicts meter-scale laboratory earthquakes. [PDF]
Norisugi R, Kaneko Y, Rouet-Leduc B.
europepmc +1 more source
Intrinsic factors responsible for brittle versus ductile nature of refractory high-entropy alloys. [PDF]
Tsuru T +9 more
europepmc +1 more source
Evidence of megathrust earthquakes and seismic supercycles in subtropical Japan from millennia-old coral microatolls. [PDF]
Debaecker S +12 more
europepmc +1 more source
Seismogenic strength and anatomy of mahendragarh-dehradun fault: implication to seismic risk. [PDF]
Gera SK +4 more
europepmc +1 more source
Thrust-dominated unilateral rupture of a blind listric fault associated with the 2024 Hualien earthquake. [PDF]
Zheng A +6 more
europepmc +1 more source
Related searches:
Afterslip, Tremor, and the Denali Fault Earthquake
Bulletin of the Seismological Society of America, 2012We 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, 1991We 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

