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Journal ArticleDOI

Evidence for and implications of self-healing pulses of slip in earthquake rupture

TLDR
In this article, a qualitative model is presented that produces self-healing slip pulses, which is the key feature of the model is the assumption that friction on the fault surface is inversely related to the local slip velocity, and the model has the following features: high static strength of materials (kilobar range), low static stress drops (in the range of tens of bars).
About
This article is published in Physics of the Earth and Planetary Interiors.The article was published on 1990-11-01. It has received 901 citations till now. The article focuses on the topics: Slip (materials science) & Earthquake rupture.

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Citations
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Book ChapterDOI

Earthquakes, Fracture, Complexity

TL;DR: The classic approach to understanding earthquakes is to apply laboratory derived rate and state dependent friction laws and to model the stickslip cycle on a planar fault embedded in an elastic media as discussed by the authors.
Book ChapterDOI

Dramatic Weakening and Embrittlement of Intact Hard Rocks in the Earth’s Crust at Seismic Depths as a Cause of Shallow Earthquakes

Boris Tarasov
TL;DR: In this paper, the authors discussed a recently identified shear rupture mechanism operating in hard rocks under high σ3 which causes dramatic rock weakening and embrittlement during the post-peak failure.
References
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Journal ArticleDOI

The Determination of the Elastic Field of an Ellipsoidal Inclusion, and Related Problems

TL;DR: In this paper, it is shown that to answer several questions of physical or engineering interest, it is necessary to know only the relatively simple elastic field inside the ellipsoid.
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Tectonic stress and the spectra of seismic shear waves from earthquakes

TL;DR: In this paper, an earthquake model is derived by considering the effective stress available to accelerate the sides of the fault, and the model describes near and far-field displacement-time functions and spectra and includes the effect of fractional stress drop.
Journal ArticleDOI

Theoretical basis of some empirical relations in seismology

TL;DR: In this article, an empirical relation involving seismic moment M, energy E, magnitude M, and fault dimension L (or area S) is discussed on the basis of an extensive set of earthquake data (M_S ≧ 6) and simple crack and dynamic dislocation models.
Journal ArticleDOI

Modeling of rock friction: 1. Experimental results and constitutive equations

TL;DR: In this paper, it is shown that the strength of the population of points of contacts between sliding surfaces determines frictional strength and that the number of contacts changes continuously with displacements.