Study of the Correlations Between Long-Periodic Terrestrial Tides and Occurrence of Earthquakes in the Vrancea Site |
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Authors: | Souchay J Stavinschi M |
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Institution: | (1) Observatoire de Paris, UMR 8630, 61, av. de l'observatoire, 75 014 Paris, France;(2) Institul Astronomic Romaniei, Str. cutitul de argint 5, Bucharest, Romania |
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Abstract: | Following studies already performed by various authors concerning specific tectonic faults we analyse statistically the possibility
that earthquakes in the very active seismological zone of Vrancea (Roumania) may be triggered by the vertical luni-solar tidal
oscillations when retaining only the components other than diurnal and semi-diurnal. Our conclusion is that for three of the
four leading tides, with periods 18.6 y, 182.62 d, and 13.66 d, the earthquakes occur preferentially during the ascending
part of each of the sine oscillation. This property is especially visible for the leading 13.66 d fortnightly wave, and for
the 18.6 y wave, for which results are very similar to that of Kilston and Knopoff (1983), who analyzed data related to the
San Andreas fault in Southern California. As a complement, we carried out an analysis of earthquake periodicities w.r.t. the
variation rate of each of the tides above, given by the half-period sine oscillation, which also leads to interesting possible
correlations.
This revised version was published online in July 2006 with corrections to the Cover Date. |
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Keywords: | Earthquakes tides |
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