Highly variable coastal deformation in the 2016 MW7.8 Kaikoura earthquake reflects rupture complexity along a transpressional plate boundary

Coseismic coastal deformation is often used to understand slip on offshore faults in large earthquakes but in the 2016 M(W)7.8 KaikOura earthquake multiple faults ruptured across and sub-parallel to the coastline. Along similar to 110 km of coastline, a rich dataset of coastal deformation comprising airborne lidar differencing, field surveying and satellite geodesy reveals highly variable vertical displacements, ranging from -2.5 to 6.5 m. These inform a refined slip model for the Kaikoura earthquake which incorporates changes to the slip on offshore faults and inclusion of an offshore reverse crustal fault that accounts for broad, low-amplitude uplift centered on Kaikoura Peninsula. The exceptional detail afforded by differential lidar and the high variability in coastal deformation combine to form the highest-resolution and most complex record of coseismic coastal deformation yet documented. This should prompt reassessment of coastal paleoseismic records that may not have considered multi-fault ruptures and high complexity deformation fields. (C) 2017 The Authors. Published by Elsevier B.V.