Small electric and magnetic signals observed before the arrival of seismic wave

Electric and magnetic data were obtained above the focal area in association with the 1999 Izmit, Turkey earthquake. The acquired data are extremely important for studies of electromagnetic phenomena associated with earthquakes, which have attracted much attention even without clear physical understanding of their characteristics. We have already reported that large electric and magnetic variations observed during the earthquake were simply due to seismic waves through the mechanism of seismic dynamo effect, because they appeared neither before nor simultaneously with the origin time of the earthquake but a few seconds later, with the arrival of seismic wave. In this letter we show the result of our further analyses. Our detailed examination of the electric and magnetic data disclosed small signals appearing less than one second before the large signals associated with the seismic waves. It is not yet solved whether this observational fact is simply one aspect of the seismic dynamo effect or requires a new mechanism.

[1]  Y. Iio Observations of the slow initial phase generated by microearthquakes: Implications for earthquake nucleation and propagation , 1995 .

[2]  T. Ishido,et al.  Electrokinetic phenomena associated with earthquakes , 1976 .

[3]  Yoichi Sasai,et al.  Application of the Elasticity Theory of Dislocations to Tectonomagnetic Modelling , 1980 .

[4]  D. Jackson,et al.  Detection of tectonomagnetic events using multichannel predictive filtering , 1981 .

[5]  Mustafa Aktar,et al.  The 1999 İzmit Earthquake Sequence in Turkey: Seismological and Tectonic Aspects , 2002 .

[6]  M. Johnston,et al.  36 Implications of crustal strain during conventional, slow, and silent earthquakes , 2002 .

[7]  M. Matsushima,et al.  Preliminary results of multidisciplinary observations before, during and after the Kocaeli (Izmit) earthquake in the western part of the North Anatolian Fault Zone , 2000 .

[8]  Steven R. Pride,et al.  Electroseismic waves from point sources in layered media , 1997 .

[9]  Frank D. Stacey,et al.  Theory of the piezomagnetic effect in titanomagnetite-bearing rocks , 1972 .

[10]  Naum I. Gershenzon,et al.  On the electromagnetic field of an earthquake focus , 1993 .

[11]  N. Puspito,et al.  Geoelectric potential difference monitoring in southern Sumatra, Indonesia — Co-seismic change— , 2000 .

[12]  M. Matsushima,et al.  Seismoelectromagnetic Effect Associated with the İzmit Earthquake and Its Aftershocks , 2002 .

[13]  T. Nagao,et al.  Co‐seismic geoelectric potential changes observed in Japan , 2000 .

[14]  Y. Honkura,et al.  Local Anomaly in Magnetic and Electric Field Variations Due to a Crustal Resistivity Change Associated with Tectonic Activity , 1986 .

[15]  T. Ishido,et al.  Experimental and theoretical basis of electrokinetic phenomena in rock‐water systems and its applications to geophysics , 1981 .

[16]  Y. Honkura,et al.  Estimation of electric fields in the conducting Earth's crust for oscillating electric current dipole sources and implications for anomalous electric fields associated with earthquakes , 1993 .

[17]  T. Hashimoto,et al.  Co-Seismic Geomagnetic Variations Observed at the 1995 Hyogoken-Nanbu Earthquake , 1996 .