Talc-bearing serpentinite and the creeping section of the San Andreas fault
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature06064.pdf
Reference30 articles.
1. Titus, S. J., DeMets, C. & Tikoff, B. Thirty-five-year creep rates for the creeping segment of the San Andreas fault and the effects of the 2004 Parkfield earthquake: Constraints from alignment arrays, continuous global positioning system, and creepmeters. Bull. Seismol. Soc. Am. 96, (4B)S250–S268 (2006)
2. Provost, A.-S. & Houston, H. Orientation of the stress field surrounding the creeping section of the San Andreas fault: Evidence for a narrow mechanically weak fault zone. J. Geophys. Res. 106, 11373–11386 (2001)
3. Hickman, S. & Zoback, M. Stress orientations and magnitudes in the SAFOD pilot hole. Geophys. Res. Lett. 31 L15S12 doi: 10.1029/2004GL020043 (2004)
4. Chéry, J., Zoback, M. D. & Hickman, S. A mechanical model of the San Andreas fault and SAFOD Pilot Hole stress measurements. Geophys. Res. Lett. 31 L15S13 doi: 10.1029/2004GL019521 (2004)
5. Williams, C. F., Grubb, F. V. & Galanis, S. P. Heat flow in the SAFOD pilot hole and implications for the strength of the San Andreas Fault. Geophys. Res. Lett. 31 L15S14 doi: 10.1029/2003GL019352 (2004)
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