Electrical resistivity structure at the SAFOD site from magnetotelluric exploration
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- Martyn Unsworth
- Institute for Geophysical Research, Department of Physics University of Alberta Edmonton, Alberta Canada
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- Paul A. Bedrosian
- GeoForschungsZentrum Potsdam Germany
書誌事項
- 公開日
- 2004-05-18
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2003gl019405
- 公開者
- American Geophysical Union (AGU)
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説明
<jats:p>The magnetotelluric dataset collected on the San Andreas Fault at Parkfield has been re‐analyzed using superior inversion algorithms that have been developed in recent years. A combination of constrained inversion, forward modeling and synthetic inversion studies are used, and show that at the SAFOD site, the low resistivity fault zone extends to a depth of 2–3 km. An extended zone of low resistivity east of the San Andreas Fault may be connected to the SAF at seismogenic depths. The connection increases along the SAF to the northwest and may be related to the transition from locked to creeping seismic behavior.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 31 (12), L12S05-, 2004-05-18
American Geophysical Union (AGU)
