Some results of gradient electromagnetic sounding in Doldrums Mid-Atlantic Ridge fracture

Details Some results of gradient electromagnetic sounding in Doldrums Mid-Atlantic Ridge fracture Some results of gradient electromagnetic sounding in Doldrums Mid-Atlantic Ridge fracture

Apr 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991pepi...66..259s&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 66, Issue 3-4, p. 259-264.

Physics

4

Scientific paper

The geoelectrical cross-section of the Doldrums Mid-Atlantic Ridge fracture has been investigated by means of the gradient electromagnetic sounding method.
The method of experiment at sea, observation techniques, principles of processing and interpretation of the observed data are described. As a result, the first model of the deep geoelectrical structure of the ridge zone, with a high conducting layer at a depth of 30 km, has been constructed.

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