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Evidence of underground electric current generation during the 2009 L'Aquila earthquake: Real or instrumental?
Author(s) -
Masci F.,
Thomas J. N.
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl069759
Subject(s) - magnetometer , offset (computer science) , magnetic field , waveform , geology , electromagnetic induction , epicenter , seismology , signal (programming language) , geodesy , earthquake prediction , geophysics , electric field , transient (computer programming) , acoustics , physics , nuclear magnetic resonance , voltage , computer science , electromagnetic coil , quantum mechanics , programming language , operating system
We investigate magnetic effects in correspondence of the M w 6.1 L'Aquila earthquake. Magnetic and seismic records are analyzed. Rapid and distinct changes and an offset can be seen in magnetic field components after the main shock. We show that these effects result from electromagnetic induction due to the movement of the sensors through the Earth's magnetic field and from a permanent displacement of the sensors from their original position caused by the passing seismic waves. A transient signal in total field data from an overhauser magnetometer apparently occurs in correspondence with the earthquake. Our analysis shows that the transient was not observed by other sensors that were operating in close proximity to the overhauser. Thus, the transient signal in the total magnetic field data, and the offset in the magnetic field components, cannot be associated with a hypothetical underground electric current generated by the earthquake, as suggested by Nenovski (2015).