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The top documents tagged [fault interaction]
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fault interaction
Geologic hazards & space geodesy part 1: Introduction.
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ss= * +(a-b) ln(V/V * ) a-b > 0 stable sliding a-b < 0 slip is potentially unstable Correspond to T~300 °C For Quartzo- Feldspathic rocks Stationary.
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Earthquake Sensation: integrating GPS and inertial sensors Kenneth W. Hudnut, Ph.D. Chief, So. Calif. Earthquake Hazard Assessment Project Earthquake Hazards.
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Kenneth W. Hudnut U. S. Geological Survey Pasadena, California Berkeley Seismo Lab Seminar U. C. Berkeley, California March 11, 2003 Measuring Fault Slip.
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Kenneth W. Hudnut U. S. Geological Survey Pasadena, California
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