TheKekerengu Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It is closely associated with theHope Fault and Jordan Thrust at its south-easternmost edge and likely joins with theClarence Fault to form theWairarapa Fault offshore inCook Strait.[1][2]
Early investigations immediately following the 14 November2016 Kaikōura earthquake indicated that up to 10 m (33 ft) of motion may have occurred on the Kekerengu Fault during the 7.8 magnitude quake.[3] The maximum displacement was later found to be 12.0 m (39.4 ft) ± 0.7 m (2 ft 4 in).[4] During this earthquake the offshore continuation of the Kekerengu Fault to the north east, known as the Needles Fault, ruptured as well.NIWA marine geologist Dr Philip Barnes said the length of the Kekerengu–Needles Fault rupture may extend for about 70 km (43 mi), consisting of 36 km (22 mi) on land and 34 km (21 mi) under the sea.[5]
^Zachariasen, Judith; Berryman, Kelvin; Langridge, Robert; Prentice, Caro; Rymer, Michael; Stirling, Mark; Villamor, Pilar (2006). "Timing of late Holocene surface rupture of the Wairau Fault, Marlborough, New Zealand".New Zealand Journal of Geology and Geophysics.49 (1):159–174.doi:10.1080/00288306.2006.9515156.
^Lensen, G.J. (1958). "Note on fault correlations across Cook Strait".New Zealand Journal of Geology and Geophysics.1 (2):263–268.doi:10.1080/00288306.1958.10423182.
