Coulomb stress changes in the South Iceland Seismic Zone due to two large earthquakes in June 2000
- 5 March 2003
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 30 (5)
- https://doi.org/10.1029/2002gl016495
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- Triggered fault slip on June 17, 2000 on the Reykjanes Peninsula, SW‐Iceland captured by radar interferometryGeophysical Research Letters, 2003
- Behaviour of a rupture of the 21 June 2000 earthquake in South Iceland as revealed in an asphalted car parkJournal of Structural Geology, 2002
- Pore fluid pressure, apparent friction, and Coulomb failureJournal of Geophysical Research, 2000
- Crustal deformation near Hengill volcano, Iceland 1993–1998: Coupling between magmatic activity and faulting inferred from elastic modeling of satellite radar interferogramsJournal of Geophysical Research, 2000
- Introduction to Special Section: Stress Triggers, Stress Shadows, and Implications for Seismic HazardJournal of Geophysical Research, 1998
- Stress transferred by the 1995Mw= 6.9 Kobe, Japan, shock: Effect on aftershocks and future earthquake probabilitiesJournal of Geophysical Research, 1998
- The 1994–1995 seismicity and deformation at the Hengill triple junction, Iceland: Triggering of earthquakes by minor magma injection in a zone of horizontal shear stressJournal of Geophysical Research, 1997
- Response of Long Valley Caldera to theMw= 7.3 Landers, California, EarthquakeJournal of Geophysical Research, 1995
- Transient stresses at Parkfield, California, produced by the M 7.4 Landers earthquake of June 28, 1992: Observations from the UPSAR dense seismograph arrayJournal of Geophysical Research, 1995
- Some basic stress diffusion solutions for fluid‐saturated elastic porous media with compressible constituentsReviews of Geophysics, 1976