2016
DOI: 10.1016/j.jog.2016.01.002
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Investigating viscoelastic postseismic deformation due to large earthquakes in East Anatolia, Turkey

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Cited by 4 publications
(1 citation statement)
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“…However, depending on the geometry of the faults, the seismic hazard represented by stress changes, with following rupture on the neighbouring faults either brought forward in time or delayed (McCloskey et al, 2005). A key element in the stress calculation is the knowledge of the elapsed time since the last damaging earthquake, as the stress renewal process, whereby faults are re-loaded either by regional stress or viscoelastic stress (Sunbul et al, 2016). Among those unknowns, one approach to the problem is determining to what extent an earthquake may influence successive events by utilizing static Coulomb stress calculations (King et al, 1994;McCloskey et al, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…However, depending on the geometry of the faults, the seismic hazard represented by stress changes, with following rupture on the neighbouring faults either brought forward in time or delayed (McCloskey et al, 2005). A key element in the stress calculation is the knowledge of the elapsed time since the last damaging earthquake, as the stress renewal process, whereby faults are re-loaded either by regional stress or viscoelastic stress (Sunbul et al, 2016). Among those unknowns, one approach to the problem is determining to what extent an earthquake may influence successive events by utilizing static Coulomb stress calculations (King et al, 1994;McCloskey et al, 2003).…”
Section: Introductionmentioning
confidence: 99%