| Title | Some new investigations of earthquake mechanism |
| Download | Download (whole publication) |
| Author | Keylis-Borok, V I |
| Source | A symposium on earthquake mechanism; by Hodgson, J H (ed.); Publications of the Dominion Observatory vol. 24, no. 10, 1961 p. 335-341, https://doi.org/10.4095/313003 (Open Access) |
| Year | 1961 |
| Publisher | Canada Department of Mines and Technical Surveys |
| Meeting | International Union of Geodesy and Geophysics, Association of Seismology and Physics of the Earth's Interior, Twelfth General Assembly; Helsinki; FI; 1960 |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| Related | This publication is contained in Hodgson, J H; (1961). A
symposium on earthquake mechanism, Publications of the Dominion Observatory vol. 24 no. 10 |
| File format | pdf |
| Subjects | geophysics; tectonics; mathematical and computational geology; seismology; earthquakes; earthquake mechanisms; crustal movements; displacement; faults; seismic waves; models; stress analyses;
seismological network; methodology |
| Illustrations | spectra; geoscientific sketch maps; graphs; tables |
| Viewing | |
| Natural Resources Canada Library - Ottawa (Earth Sciences) |
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| Released | 1961 01 01; 2018 11 19 |
| Abstract | 1. Theory predicts that in azimuths coinciding with the fault strike, the maximum in the surface-wave spectrum is at a higher period than in perpendicular azimuths. This can be used together with body
waves or independently for fault-plane determinations.
2. A method is considered which permits one to investigate the selectivity of a system of stations used in fault-plane studies. The method also simplifies subsequent interpretation.
3.
Some simplified methods to obtain a source model are investigated. A model, obtained by analogy with dislocation theory, is shown to correspond to a peculiar distribution of pre-faulting stress which cannot correspond to a real source. |
| GEOSCAN ID | 313003 |
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