Coseismic deformation of the 2002 Denali Fault earthquake: Insights from GPS measurements

Author:

Hreinsdóttir Sigrún1,Freymueller Jeffrey T.1,Bürgmann Roland2,Mitchell Jim3

Affiliation:

1. Geophysical Institute; University of Alaska Fairbanks; Fairbanks Alaska USA

2. Department of Earth and Planetary Science; University of California; Berkeley California USA

3. The Crazy Mountains Joint Venture; Anchorage Alaska USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference43 articles.

1. Geophys. Monogr. Ser.;Bakun,1986

2. Near-source modeling of the Loma Prieta earthquake: Evidence for heterogeneous slip and implications for earthquake hazard;Beroza;Bull. Seismol. Soc. Am.,1991

3. Boucher , C. Z. Altamimi P. Sillard 1999 The 1997 International Terrestrial Reference Frame (ITRF97) IERS Tech. Note 27 Int. Earth Rotation Serv. Paris

4. The state of stress on some faults of the San Andreas system as inferred from near-field strong motion data;Bouchon;J. Geophys. Res.,1997

5. Coseismic and early post-seismic slip associated with the 1999 Izmit earthquake (Turkey), from SAR interferometry and tectonic field observations;Çakir;Geophys. J. Int.,2003

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