| Abstract: | In this model for the evolution of large crustal faults, water originally from the country rock saturates the porous and permeable fault zone. During shearing, the fault zone compacts and water flows back into the country rock, but the flow is arrested by silicate deposition that forms low permeability seals. The fluid will be confined to seal-bounded fluid compartments of various sizes and porosity that are not hydraulically connected with each other. When the seal between two compartments is ruptured, an electrical streaming potential will be generated by the sudden movement of fluid from the high-pressure compartment to the low-pressure compartment. During an earthquake the width of the fault zone will increase by failure of the geometric irregularities on the fault. This newly created, porous and permeable, wider fault zone will fill with water, and the process described above will be repeated. Thus, the process is episodic with the water moving in and out of the fault zone, and each large earthquake should be preceded by an electrical and/or magnetic signal. -from Author |
| Genre: | Article |
| ProdID: | 70018333 |
| Citation Author: | Byerlee, J. |
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| Citation End Page: | 306 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Model for episodic flow of high-pressure water in fault zones before earthquakes; 1993; Article; Journal; Geology; Byerlee, J. |
| Citation Start Page: | 303 |
| Citation Volume: | 21 |
| Citation Year: | 1993 |
| Type: | citation/reference |
| Text: | Model for episodic flow of high-pressure water in fault zones before earthquakes; 1993; Article; Journal; Geology; Byerlee, J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Fri, 1 Jan 1993 00:00 -0600 |
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