Source mechanism of the Alaskan earthquake of 1964 from amplitudes of free oscillations and surface waves - comments

Details Source mechanism of the Alaskan earthquake of 1964 from amplitudes of free oscillations and surface waves - comments Source mechanism of the Alaskan earthquake of 1964 from amplitudes of free oscillations and surface waves - comments

Jun 1973

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1973pepi....7..222k&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 7, Issue 2, p. 222-224.

Physics

Scientific paper

Recently Ben-Menahem et al. (1972) (hereafter abbreviated to B.R.I.) proposed, on the basis of long-period surface-wave and free-oscillation data, a steeply dipping fault model for the Alaskan earthquake of 1964. This result differs from that obtained by Kanamori (1970) (hereafter abbreviated to K.70) who also used long-period Love and Rayleigh waves, but preferred a low-angle fault model. I would like to make several comments on this difference. Present address: Seismological Laboratory, California Institute of Technology, Pasadena, Calif., U.S.A.

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