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Geology; January 2003; v. 31; no. 1; p. 55-58; DOI: 10.1130/0091-7613(2003)031\|[lt ]\|0055:PAGPSE\|[gt ]\|2.0.CO;2
© 2003 Geological Society of America
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Paleoseismology and Global Positioning System: Earthquake-cycle effects and geodetic versus geologic fault slip rates in the Eastern California shear zone

Timothy H. Dixon1, E. Norabuena1 and L. Hotaling2

1 Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149, USA
2 Department of Geological Sciences, University of Miami, Miami, Florida 33124, USA

Published slip rates for the Owens Valley fault zone in eastern California based on geodetic data and elastic half-space models (5–7 mm/yr) are faster than longer term geologic rates (2–3 mm/yr). We use Global Positioning System data spanning the central Owens Valley, a more realistic rheological model with an elastic upper crust over a viscoelastic lower crust and upper mantle, and paleoseismic data from adjacent faults, to show that this difference could reflect earthquake-cycle effects. We estimate a long-term rate (2.1 ± 0.7 mm/yr) and earthquake recurrence interval (2750 +350/–1000 yr) from the geodetic data, both in agreement with independent geologic estimates.

Key Words: GPS • earthquake cycle • paleoseismology • fault slip rates




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