Tomography of seismo-radio wave source regions for predicting imminent earthquakes

Details Tomography of seismo-radio wave source regions for predicting imminent earthquakes Tomography of seismo-radio wave source regions for predicting imminent earthquakes

Oct 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989pepi...57...40t&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 57, Issue 1-2, p. 40-44.

Physics

6

Scientific paper

To detect a seismo-electromagnetic effect in a noisy land area or a deep-sea area, two methods are proposed. In the land area, a steel casing pipe inserted in a deep borehole has been used as the linear element of a monopole antenna. This method is shown to be very effective in rejecting atmospherics. In the deep-sea area, man-made noise and atmospherics can be attenuated by using insulated cables extended along the seabed as a dipole antenna or a loop antenna. Taking advantage of the seismo-radio wave propagating directly through the Earth's crust, a tomography is proposed to describe a three-dimensional intensity distribution of seismo-radio wave sources by receiving the wave at four or more points simultaneously, to predict precisely an earthquake of magnitude seven or more.

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