Fig. 7From: Coseismic and postseismic deformation associated with the 2016 Mw 7.8 Kaikoura earthquake, New Zealand: fault movement investigation and seismic hazard analysisCoseismic Coulomb stress changes in the mainshock regions. a–c Coseismic Coulomb stress changes corresponding to 1, 9, and 17 km depth, which reflect Coulomb stress changes on shallow receiver faults. d Coseismic Coulomb stress changes at 35 km depth at the southwestern Hikurangi subduction interface. The dark gray dots are the aftershocks based on the GeoNet earthquake catalogueBack to article page