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Slip Rate on the Wellington Fault, New Zealand, during the Late Quaternary: Evidence for Variable Slip during the HoloceneDee Ninis, C M Henderson, Timothy A. Little et al.|Bulletin of the Seismological Society of America|2013Cited by 28
It's Our Fault: Better Defining Earthquake Risk in WellingtonRuss Van Dissen, John X. Zhao, Bill Fry et al.|University of Canterbury Research Repository (University of Canterbury)|2010Cited by 14
Causes of permanent vertical deformation at subduction margins: Evidence from late Pleistocene marine terraces of the southern Hikurangi margin, Aotearoa New ZealandDee Ninis, Nicola Litchfield, Andy Howell et al.|Frontiers in Earth Science|2023Cited by 11
Pleistocene marine terraces of the Wellington south coast – their distribution across multiple active faults at the southern Hikurangi subduction margin, Aotearoa New ZealandDee Ninis, C M Henderson, Timothy A. Little et al.|New Zealand Journal of Geology and Geophysics|2022Cited by 9