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Phys. Rev. Lett. 91, 148501 (2003) [4 pages]

Electric Fields that “Arrive” before the Time Derivative of the Magnetic Field prior to Major Earthquakes

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P. A. Varotsos1,2,*, N. V. Sarlis1, and E. S. Skordas1,2
1Solid State Section, Physics Department, University of Athens, Panepistimiopolis, Zografos 157 84, Athens, Greece
2Solid Earth Physics Institute, Physics Department, University of Athens, Panepistimiopolis, Zografos 157 84, Athens, Greece

Received 12 February 2003; published 3 October 2003

The low frequency electric signals (emitted from the focal area when the stress reaches a critical value) that precede major earthquakes, are recorded at distances ≈100   km being accompanied by magnetic field variations. The electric field “arrives” 1 to 2 s before the time derivative of the horizontal magnetic field. An explanation, which is still awaiting, should consider, beyond criticality, the large spatial scale as well as that the transmission of the electromagnetic fields (through an inhomogeneous weakly conductive medium like the Earth) obeys diffusion type equations.

© 2003 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevLett.91.148501
DOI:
10.1103/PhysRevLett.91.148501
PACS:
91.30.–f, 03.50.De, 05.40.–a, 41.20.–q

*Electronic address: pvaro@otenet.gr