Hundalee Fault, North Canterbury, New Zealand: Late Quaternary activity and regional tectonics_Supplementary Information

This document is a Supplement to the paper:

Barrell, DJA, Stirling MW, Williams JN, Sauer KM, van den Berg E. Hundalee Fault, North Canterbury, New Zealand: Late Quaternary activity and regional tectonics. New Zealand Journal of Geology and Geophysics. Special issue: Kaikōura earthquake 5 years on. 

This Supplement begins with a review and assessment of information on the Holocene and Pleistocene terraces along the Conway section of the North Canterbury coast (Sections S1 and S2). The purpose is to assess whether previous estimates of coastal uplift rates, some dating back to the mid-1980s, especially Ota et al. (1984), still remain appropriate in light of more recent information. This is followed by description and assessment of the Okarahia valley fluvial terrace sequence (Section S3). Section S4 describes structural modelling, Section S5 discusses Kaikōura Peninsula marine terraces and structural interpretation, and Section S6 discusses aftershock distributions.