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- W2018181921 abstract "The magnetic field near a vertical alternating magnetic dipole on the surface of a layered earth is computed for points on the surface. In the layer the dimensionless conductivity parameter is assumed to take the values 0, [Formula: see text], 1, and 4; in the homogeneous substratum, this parameter is assigned the values 0, [Formula: see text], 1, 4, and infinity. The induced field is computed at distances from the source [Formula: see text], 1, 2, 4, 8, and 16 times the layer thickness." @default.
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- W2018181921 date "1959-02-01" @default.
- W2018181921 modified "2023-09-27" @default.
- W2018181921 title "FIELD OF AN ALTERNATING MAGNETIC DIPOLE ON THE SURFACE OF A LAYERED EARTH" @default.
- W2018181921 doi "https://doi.org/10.1190/1.1438570" @default.
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