A magnetotelluric experiment in Nozay-en-Dunois (Eure-et-Loir, France): Results, interpretation and critical study

Details A magnetotelluric experiment in Nozay-en-Dunois (Eure-et-Loir, France): Results, interpretation and critical study A magnetotelluric experiment in Nozay-en-Dunois (Eure-et-Loir, France): Results, interpretation and critical study

Feb 1974

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974pepi....8...13f&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 8, Issue 1, p. 13-18.

Physics

3

Scientific paper

The results of a two months' field experiment are presented. As the variations of the vertical component of the earth's magnetic field are relatively small, we can infer that we have a layered system. This hypothesis is shown indirectly to be correct since the impedance is independent of the direction of the electric vector. We suggest an interpretation model which requires two intermediate conductive layers.

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