Coseismic stress changes and crustal deformation on the Reykjanes Peninsula due to triggered earthquakes on 17 June 2000

Author:

Árnadóttir Thóra1,Geirsson Halldór2,Einarsson Páll3

Affiliation:

1. Nordic Volcanological Institute; Reykjavík Iceland

2. Icelandic Meteorological Office; Reykjavík Iceland

3. Science Institute; University of Iceland; Reykjavík Iceland

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

Reference42 articles.

1. Seismic swarms and surface deformation in the Hengill area, SW Iceland;Árnadóttir;Seismol. Res. Lett.,1999

2. Árnadóttir , T. H. Geirsson B. H. Bergsson C. Völksen 2000 The Icelandic continuous GPS network-ISGPS, March 18, 1999-February 20, 2000 VI-R00002-JA02 Icelandic Meteorol. Off. Reykjavík

3. Crustal deformation measured by GPS in the South Iceland Seismic Zone due to two large earthquakes in June 2000;Árnadóttir;Geophys. Res. Lett.,2001

4. Coulomb stress changes in the South Iceland Seismic Zone due to two large earthquakes in June 2000;Árnadóttir;Geophys. Res. Lett.,2003

5. Pore fluid pressure, apparent friction, and Coulomb failure;Beeler;J. Geophys. Res.,2000

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