| Abstract: | Episodic slip on shallow crustal faults can be qualitatively explained by postulating a fault constitutive law that is the superposition of two limiting material responses: (1) strain softening after peak stress during large strain rates, and (2) strength (peak stress) recovery during aging at small strain rates. A single law permits a variety of seismic and aseismic phenomena to occur over a range of space and time scales. Specific cases are determined by the spatial variation of material constants, recent deformation history, crustal rigidity, and remote forcing. ?? 1979. |
| Genre: | Article |
| ProdID: | 70012502 |
| Citation Author: | Stuart, W. D. |
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| Citation End Page: | 626 |
| Citation Issue: | 1-4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Tectonophysics |
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| Citation Number Of Pages: | 14 |
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| Citation Search Results Text: | Aging and strain softening model for episodic faulting; 1979; Article; Journal; Tectonophysics; Stuart, W. D. |
| Citation Start Page: | 613 |
| Citation Volume: | 52 |
| Citation Year: | 1979 |
| Type: | citation/reference |
| Text: | Aging and strain softening model for episodic faulting; 1979; Article; Journal; Tectonophysics; Stuart, W. D. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Mon, 1 Jan 1979 00:00 -0600 |
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