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Some relationships between VAN Seismic Electric Signals (SES) and earthquake parameters: study for the 1995-2007 period

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EN
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A 12-year period experimental data, from 1 January 1995, to 20 August 2007, have been examined for possible correlations between Seismic Electric Signals (SES) of the VAN method and source parameters of the corresponding earthquakes in Western Greece. During that period 13 earthquakes of magnitude M W //5 with epicenters in the area 19–24°E, 36–41°N and available the CMT solutions (Centroid Moment Tensor focal mechanism solutions) have been found to be preceded by a SES each time at one of the three VAN stations of IOA, PIR or PAT. The results of IOA and PIR stations are compared to those reported by Uyeda et al. 1999, for the previous period 1983–1994. The IOA station seems to be sensitive to earthquakes with thrust type mechanisms being mainly consistent to its past behavior. The PIR station, which is moved from its previous position by few kilometers, exhibits some changes. It detects now both strike slip and thrust type earthquakes and becomes sensitive to new areas indicating probably the strong dependence of the SES station detection ability upon its location.
Czasopismo
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1015--1024
Opis fizyczny
Bibliogr. 27 poz.
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Bibliografia
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  • Uyeda, S., K.S. Al-Damegh, E. Dologlou, and T. Nagao (1999), Some relationship between VAN seismic electric signals (SES) and earthquake parameter, Tectonophysics 304, 41-56, DOI: 10.1016/S0040-1951(98)00301-1.
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  • Varotsos, P., and K. Alexopoulos (1984b), Physical properties of the variations of the electric field of the earth preceding earthquakes. II: Determination of epicentre and magnitude, Tectonophysics 110, 99-125, DOI: 10.1016/0040-1951(84)90060-X.
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  • Varotsos, P., and M. Lazaridou (1991), Latest aspects of earthquake prediction in Greece based on Seismic Electric Signals, Tectonophysics 188, 321-347, DOI: 10.1016/0040-1951(91)90462-2.
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  • Varotsos, P., K. Alexopoulos, and M. Lazaridou (1993), Latest aspect of earthquake prediction in Greece based on Seismic Electric Signals II, Tectonophysics 224, 1-37, DOI: 10.1016/0040-1951(93)90055-O.
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  • Varotsos, P., N. Sarlis, and E. Skordas (2001), Spatiotemporal complexity aspects on the interrelation between Seismic Electric Signals and seismicity, Practica of Athens Academy 76, 294-321.
  • Varotsos, P.A., N.V. Sarlis, and E.S. Skordas (2002), Long-range correlations in the electric signals that precede rupture, Phys. Rev. E 66, 011902, DOI: 10.1103/PhysRevE.66.011902.
  • Varotsos, P.A., N.V. Sarlis, and E.S. Skordas (2003a), Long-range correlations in the electric signals that precede rupture: Further investigations, Phys. Rev. E 67, 021109, DOI: 10.1103/PhysRevE.67.021109.
  • Varotsos, P.A., N.V. Sarlis, and E.S. Skordas (2003b), Attempt to distinguish electric signals of a dichotomous nature, Phys. Rev. E 68, 031106, DOI: 10.1103/PhysRevE.68.031106
  • Varotsos, P., N. Sarlis, E. Skordas, and M. Lazaridou (2006a), Additional evidence on some relationship between Seismic Electric Signals (SES) and earthquakefocal mechanism, Tectonophysics 412, 279-288, DOI: 10.1016/ j.tecto.2005.10.037.
  • Varotsos, P.A., N.V. Sarlis, E.S. Skordas, H.K. Tanaka, and M.S. Lazaridou 2006b), Attempt to distinguish long-range temporal correlations from he statistics of the increments by natural time analysis, Phys. Rev. E 74, 21123, DOI: 10.1103/PhysRevE.74.021123
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Typ dokumentu
Bibliografia
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bwmeta1.element.baztech-article-BSL7-0028-0026
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