Coulomb stress changes in the South Iceland Seismic Zone due to two large earthquakes in June 2000

Author:

Árnadóttir Thóra1,Jónsson Sigurjón2,Pedersen Rikke1,Gudmundsson Gunnar B.3

Affiliation:

1. Nordic Volcanological Institute; Reykjavík Iceland

2. Harvard University; Department of Earth and Planetary Sciences; Cambridge Massachusetts USA

3. Icelandic Meteorological Office; Reykjavík Iceland

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference22 articles.

1. Behaviour of a rupture of the 21 June 2000 earthquake in south Iceland as revealed in an asphalted car park;Angelier;J. Struct. Geol.,2002

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

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

4. The 1912 Iceland earthquake rupture: Growth and development of a nascent transform system;Bjarnason;Bull. Seismol. Soc. Am.,1993

5. Björnsson , G. Ó. G. Flovenz K. Saemundsson E. M. Einarsson Pressure changes in Icelandic geothermal reservoirs associated with two large earthquakes in June 2000 26th workshop on Geothermal Reservoir Engineering Stanford Univ. Stanford, Calif. 2001

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