Kanamori, Hiroo (1973) Source mechanism of the Alaskan earthquake of 1964 from amplitudes of free oscillations and surface waves — comments. Physics of the Earth and Planetary Interiors, 7 (2). pp. 219-224. ISSN 0031-9201. doi:10.1016/0031-9201(73)90014-9. https://resolver.caltech.edu/CaltechAUTHORS:20150218-065739218
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Abstract
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.
| Item Type: | Article | |||||||||
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| Additional Information: | © 1973 Published by Elsevier B.V. Accepted 17 November 1972, Available online 11 October 2002. I benefitted from discussions with Katsuyuki Abe and Tomowo Hirasawa. | |||||||||
| Group: | UNSPECIFIED, Division of Geological and Planetary Sciences | |||||||||
| Issue or Number: | 2 | |||||||||
| DOI: | 10.1016/0031-9201(73)90014-9 | |||||||||
| Record Number: | CaltechAUTHORS:20150218-065739218 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20150218-065739218 | |||||||||
| Official Citation: | Hiroo Kanamori, Source mechanism of the Alaskan earthquake of 1964 from amplitudes of free oscillations and surface waves — comments, Physics of the Earth and Planetary Interiors, Volume 7, Issue 2, June 1973, Pages 222-224, ISSN 0031-9201, http://dx.doi.org/10.1016/0031-9201(73)90014-9. (http://www.sciencedirect.com/science/article/pii/0031920173900149) | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 54899 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | Ruth Sustaita | |||||||||
| Deposited On: | 18 Feb 2015 15:45 | |||||||||
| Last Modified: | 10 Nov 2021 20:39 |
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