Implications of deformation following the 2002 Denali, Alaska, earthquake for postseismic relaxation processes and lithospheric rheology

Author:

Freed Andrew M.,Bürgmann Roland,Calais Eric,Freymueller Jeff,Hreinsdóttir Sigrún

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

Reference84 articles.

1. ITRF2000: A new release of the International Terrestrial Reference Frame for earth science applications;Altamimi;J. Geophys. Res.,2002

2. dependent strain following faulting of a porous-medium;Booker;J. Geophys. Res.,1974

3. Aftershocks and pore fluid diffusion following the 1 992 Landers earthquake;Bosl;J. Geophys. Res.,2002

4. Seismic velocity models for the Denali Fault Zone along the Richardson Highway, Alaska;Brocher;Bull. Seismol. Soc. Am.,2004

5. Fault movement (afterslip) following the Guatemala earthquake of February 4, 1976;Buckman;Geology,1978

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