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Book ChapterDOI

Fault interaction by elastic stress changes: New clues from earthquake sequences

Geoffrey C. P. King, +1 more
- 01 Jan 2001 - 
- Vol. 44
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TLDR
In this paper, the authors present a theoretical framework for earthquake cycles based on calculating the stress changes caused by one event and assessing where and what mechanism of earthquakes these changes may promote, which is different from investigating the dynamic rupture growth requiring the reconstruction of the spatiotemporal evolution of the stress on the fault plane.
Abstract
Publisher Summary This chapter discusses the recent developments in understanding how earthquakes interact with each other. The new theoretical framework for earthquake cycles is based on calculating the stress changes caused by one event and assessing where and what mechanism of earthquakes these changes may promote. For studying such stress interaction, the computation of the stress field outside a rupturing fault is analyzed. This is different from investigating the dynamic rupture growth requiring the reconstruction of the spatiotemporal evolution of the stress on the fault plane. The chapter discusses the theoretical background of earthquake sequences and reviews some of the simple examples that allowed stress coupling concepts to be accepted. The success of simple stress modeling led to the introduction of several modifications, adaptations, and refinements of the ideas.

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Citations
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Journal ArticleDOI

Stress triggering in thrust and subduction earthquakes and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults

TL;DR: In this article, the authors argue that key features of thrust earthquake triggering, inhibition, and clustering can be explained by Coulomb stress changes, which illustrate by a suite of representative models and by detailed examples.
Journal ArticleDOI

Forecasting the evolution of seismicity in southern California: Animations built on earthquake stress transfer

TL;DR: In this article, a forecast model was developed to reproduce the distribution of main shocks, aftershocks and surrounding seismicity observed during 1986-2003 in a 300 × 310 km area centered on the 1992 M = 7.3 Landers earthquake.
Journal ArticleDOI

Earthquake triggering by static, dynamic, and postseismic stress transfer

TL;DR: In this paper, the authors used static Coulomb stress changes associated with earthquake slip to explain aftershock distributions, earthquake sequences, and the quiescence of broad, normally active regions following large earthquakes.
Journal Article

Forecasting the evolution of seismicity in southern California : Animations built on earthquake stress transfer : Stress transfer, earthquake triggering, and time-dependent seismic hazard

TL;DR: In this paper, a forecast model was developed to reproduce the distribution of main shocks, aftershocks and surrounding seismicity observed during 1986-2003 in a 300 x 310 km area centered on the 1992 M = 7.3 Landers earthquake.
Book ChapterDOI

Characterization of Fault Zones

TL;DR: There are currently three major competing views on the essential geometrical, mechanical, and mathematical nature of faults as discussed by the authors : the standard view is that faults are (possibly segmented and heterogeneous) Euclidean zones in a continuum solid.
References
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Book

Fundamentals of rock mechanics

TL;DR: In this article, Mecanique des roches and Analyse des contraintes were used to construct Elasticite Reference Record (ER) and Elasticite reference record (ER).
Journal ArticleDOI

Surface deformation due to shear and tensile faults in a half-space

TL;DR: In this paper, a suite of closed analytical expressions for the surface displacements, strains, and tilts due to inclined shear and tensile faults in a half-space for both point and finite rectangular sources are presented.
Journal ArticleDOI

Internal deformation due to shear and tensile faults in a half-space

TL;DR: A complete set of closed analytical expressions for the internal displacements and strains due to shear and tensile faults in a half-space for both point and finite rectangular sources is presented in this paper.
Journal ArticleDOI

Slip instability and state variable friction laws

TL;DR: In this paper, the dependence of the friction force on slip history is described by an experimentally motivated constitutive law where the friction forces are dependent on slip rate and state variables.
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.
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