Source parameters of large historical (1917-1961) earthquakes, North Island, New Zealand
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/152/3/795/2037024/152-3-795.pdf
Reference47 articles.
1. Arnadottir, T. , Thornley, S. , Pollitz, F.F. & Darby, D. , 1999. Spatial and temporal strain rate variations at the northern Hikurangi margin, New Zealand, J. geophys. Res., 104, 4931-4944.
2. Baker, M.R. & Doser, D. , 1988. Joint inversion of regional and teleseismic earthquake waveforms, J. geophys. Res., 93, 2037-2045.
3. Normal faulting through subducted oceanic crust: the 19 July 1985 earthquake of Hawke's Bay, New Zealand;Bannister;Tectonophysics,1989
4. Beanland, S. & Haines, A.J. , 1998. A kinematic model of active deformation in the North Island, New Zealand, determined from geological strain rates, New Zealand J. Geol. Geophys., 41, 311-323.
5. Beanland, S. , Blick, G.H. & Darby, D. , 1990. Normal faulting in a back-arc basin: geological and geodetic characteristics of the 1987 March 2 Edgecumbe earthquake, New Zealand, J. geophys. Res., 95, 4693-4707.
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