Physics
Scientific paper
Feb 1974
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974pepi....8...83l&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 8, Issue 1, p. 83-86.
Physics
2
Scientific paper
The comparison between the variations of the horizontal components of the magnetic field above the ocean and at the ocean floor leads theoretically to the same investigation capabilities as the M-T methods on the sea bed. For a model σ = f(z), we calculate the H1(t) field at the bottom of the ocean as the response to the actual H0(t) magnetic field at sea level composed of a succession of Dirac's pulses. We apply this convolution method of analysis to refnds of the magnetic declination off the Californian Coast, published by J.H. Filloux, and compare the H1(t) values computed for two structures with the D refnd of the ``sea-floor'' station. Correspondence address: Mme L. Launay, Station de Geodynamique sous-marine, La Darse, 06 - Villefranche-surmer-France.
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