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Earth, Planets and Space
Fig. 8 | Earth, Planets and Space

Fig. 8

From: Coseismic and postseismic deformation associated with the 2016 Mw 7.8 Kaikoura earthquake, New Zealand: fault movement investigation and seismic hazard analysis

Fig. 8

a Interseismic fault coupling and slow-slip regions along the Hikurangi subduction interface, modified after Wallace and Beavan (2010). b Historical earthquakes and aftershocks surrounding the Wellington region, both are based on the GeoNet earthquake catalogue. c Total CFS changes on shallow receiver faults around the Wellington region. The total CFS changes are the sum of coseismic and postseismic Coulomb stress changes. The shallow average receiver fault parameters (226° strike, 70° dip, and 160° rake) are based on the study of Robinson et al. (2011). d Total CFS changes at the Hikurangi subduction interface. The geometry of the Hikurangi subduction interface is based on the study of Williams et al. (2013)

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