Abstract
The 1993 Tikokino, New Zealand earthquake (ML 6.1) is modelled as a unilateral rupture, exhibiting clear source directivity to the south. The earthquake was recorded by four strong motion stations within 30 km: Waipawa to the south, and three sites in Napier and Hastings to the northeast. The shorter duration and greater amplitudes (by a factor of 10) observed at Waipawa with respect to the other stations provide clear evidence for the southward rupture direction.
The Tikokino earthquake occurred on a shallow dipping, oblique reverse fault, and probably represents movement at the plate interface. A high rupture velocity is required to match the distribution of observed ground shaking, and the rupture area is constrained to be c. 7 × 2 km2. The moment of the preferred model is 1.1 × 1018 Nm (Mw 6.0) and the stress drop about 35 MPa. This high average stress drop is consistent with the rupture being confined to an isolated asperity.
The model used consists of a finite, rectangular fault rupturing with prescribed velocity and direction, and with uniform slip. The fault is embedded in a planar layered seismic velocity structure. The ability of the model to match the principal features of the observed seismograms suggests that it will be a useful tool in the prediction of strong ground motion for seismic hazard studies in the region.