Coseismic strike slip at a point during the last four earthquakes on the Wellington fault near Wellington, New ZealandTimothy A. Little, R. M. Langridge, Russ Van Dissen et al.|Journal of Geophysical Research Atmospheres|2010Cited by 44
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
Quaternary deformation along the Wharekauhau fault system, North Island, New Zealand: Implications for an unstable linkage between active strike‐slip and thrust faultsElizabeth R. Schermer, U. Rieser, Timothy A. Little|Tectonics|2009Cited by 16