Proceedings of the Japan Academy, Series B
Online ISSN : 1349-2896
Print ISSN : 0386-2208
ISSN-L : 0386-2208
Volume 76, Issue 4
Displaying 1-2 of 2 articles from this issue
  • Kostas EFTAXIAS, John KOPANAS, Nikos BOGRIS, Panayiotis KAPIRIS, Georg ...
    2000 Volume 76 Issue 4 Pages 45-50
    Published: 2000
    Released on J-STAGE: October 17, 2006
    Electromagnetic (EM) anomalies were detected in a wide frequency band prior to the two strongest earthquakes that occurred in Greece during 1995, i.e., at Kozani-Grevena and Egio-Eratini areas. The analysis of these EM anomalies indicates that these EM anomalies should be pre-seismic ones. Two basic characteristics emerged: (i) The lead time of each disturbance was systematically smaller in the case of Kozani-Grevena earthquake than that of the Egio-Eratini earthquake. (ii) An almost simultaneous cessation of the EM anomalies, although they had different onset times and were detected in a wide frequency range. As for the seismic activity that occurred in Greece during the last year, pre-seismic EM anomalies were detected before (i) the September 7, 1999, Athens earthquake and (ii) other smaller EQs. The possibility to predict the parameters of an impending EQ from the EM anomalies is also investigated.
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  • Efthimios SKORDAS, Panayiotis KAPIRIS, Nikos BOGRIS, Panayiotis VAROTS ...
    2000 Volume 76 Issue 4 Pages 51-56
    Published: 2000
    Released on J-STAGE: October 17, 2006
    Simultaneous electric, magnetic and seismic measurements in Greece show that, for epicentral distances of the order of 100km and for M6 class earthquakes, no electric disturbances in the frequency range DC to 50Hz are recorded at earthquake origin time. Electric disturbances are recorded only during the arrival of seismic waves and have the following properties: (a) The amplitude does not scale with the dipole length and may significantly differ for parallel horizontal short dipoles located at neighboring sites. (b) The amplitude of the vertical component does not exceed the strongest horizontal one. (c) The data collected with a sampling rate of 50Hz, show that strong frequency content lies in the range up to around 2.5 Hz and the disturbances vanish at frequencies less than 0.1Hz and more than 5Hz, providing an explanation on the absence of these disturbances in the usual VAN real time records. These disturbances are accompanied with magnetic variations recorded either by coil and/or by torsion photoelectric magnetometers. It is not yet clear whether the magnetic variations are solely due, or not, to“vibrations”of the magnetometers upon the arrival of seismic waves. Electric disturbances were also recorded upon the arrival of seismic waves of the Izmit, Turkey, earthquake of August 17, 1999 in most of our stations. However, no pronounced electric disturbances were recorded during the Athens earthquake of September 7, 1999, neither for the Turkish event of November 12, 1999. The basic results of this paper are compatible with those reported by Uyeda et al.1)
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