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CONSTRAINING THE SLIP DISTRIBUTION AND FAULT GEOMETRY OF THE MW 7.9,3 NOVEMBER 2002, DENALI FAULT EARTHQUAKE WITH INTERFEROMETRICSYNTHETIC APERTURE RADAR AND GLOBAL POSITIONING SYSTEM DATA (2004)

The Mw 7.9, Denali fault earthquake (DFE) is the largest continental strike-slip earthquake to occur since the development of Interferometric Synthetic Aperture Radar (InSAR). We use five interferograms, constructed using radar images from the Canadian Radarsat-1 satellite, to map the surface deformation at the western end of the fault rupture.

Reference:
Bulletin of the Seismological Society of America, Vol. 94, No. 6B, pp. S175-S189, December 2004
Organization:
Centre for the Observation and Modelling of Earthquakes and TectonicsDepartment of Earth SciencesParks Road, Oxford, OX1 3PR, United Kingdom
Alaska
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