Open AccessThe 2003, Mw 7.2 Fiordland earthquake, and its near-source aftershock strong motion data
Author(s) -
Peter McGinty
Publication year - 2004
Publication title -
bulletin of the new zealand society for earthquake engineering/nzsee quarterly bulletin
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.917
H-Index - 36
eISSN - 2324-1543
pISSN - 1174-9857
DOI - 10.5459/bnzsee.37.3.139-145
Subject(s) - aftershock , attenuation , geology , seismology , subduction , magnitude (astronomy) , current (fluid) , data set , ground motion , strong ground motion , source model , tectonics , physics , computer science , oceanography , astronomy , artificial intelligence , optics , computational physics
The 2003 Fiordland earthquake was not only the best ever recorded subduction interface earthquake to occur in New Zealand, it also provided the opportunity to collect near-source strong-motion data produced by its aftershocks covering a wide magnitude range. Near source strong-motion data had been lacking in the New Zealand data set, on which current attenuation models are based. Here the author presents some preliminary results relating recorded peak ground accelerations in the near-source field to current attenuation models. The near-source data from the 2003 Fiordland earthquake sequence has shown that the observed data has a greater magnitude-dependence than that predicted by the current attenuation models. This new data will help to improve current models and will lead to a better understanding of the attenuation process associated with New Zealand subduction interface earthquakes.