Properties of inelastic yielding zones generated by in-plane dynamic ruptures—II. Detailed parameter-space study
Article first published online: 26 OCT 2012
DOI: 10.1111/j.1365-246X.2012.05685.x
© 2012 The Authors Geophysical Journal International © 2012 RAS
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How to Cite
Xu, S., Ben-Zion, Y. and Ampuero, J.-P. (2012), Properties of inelastic yielding zones generated by in-plane dynamic ruptures—II. Detailed parameter-space study. Geophysical Journal International, 191: 1343–1360. doi: 10.1111/j.1365-246X.2012.05685.x
Publication History
- Issue published online: 12 NOV 2012
- Article first published online: 26 OCT 2012
- Accepted 2012 September 19. Received 2012 July 4; in original form 2012 February 8
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Keywords:
- Microstructures;
- Elasticity and anelasticity;
- Rheology and friction of fault zones;
- Dynamics and mechanics of faulting;
- Fractures and faults;
- Mechanics, theory, and modelling
SUMMARY
We perform a detailed parameter-space study on properties of yielding zones generated by 2-D in-plane dynamic ruptures on a planar fault with different friction laws and parameters, different initial stress conditions, different rock cohesion values, and different contrasts of elasticity and mass density across the fault. The focus is on cases corresponding to large strike-slip faults having high angle (
) to the maximum compressive background stress. The simulations and analytical scaling results show that for crack-like ruptures (1) the maximum yielding zone thickness Tmax linearly increases with rupture distance L and the ratio Tmax/L is inversely proportional to (1 +S)2 with S being the relative strength parameter; (2) the potency density
decays logarithmically with fault normal distance at a rate depending on the stress state and S; (3) increasing rock cohesion reduces Tmax/L, resulting in faster rupture speed and higher inclination angle
of expected microfractures on the extensional side of the fault. For slip pulses in quasi-steady state, T is approximately constant along strike with local values correlating with the maximum slip velocity (or final slip) at a location. For a bimaterial interface with
, the energy dissipation to yielding contributes to developing macroscopically asymmetric rupture (at the scale of rupture length) with the same preferred propagation direction predicted for purely elastic cases with Coulomb friction. When
, representative for thrust faulting, the energy dissipation to yielding leads to opposite preferred rupture propagation. In all cases,
is higher on average on the compliant side. For both crack and pulse ruptures with
, T decreases and
increases for conditions representing greater depth. Significant damage asymmetry of the type observed across several large strike-slip faults likely implies persistent macroscopic rupture asymmetry (unilateral cracks, unilateral pulses or asymmetric bilateral pulses). The results on various features of yielding zones expected from this and other studies are summarized in a table along with observations from the field and laboratory experiments.

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