FIELD: geophysics, in particular, paleomagnetism.
SUBSTANCE: the position of the interfaces formed by inversions of the geomagnetic field is determined by pulse radar detection and ranging of the magnetic field with the aid of radar units with a power potential of 500 to 600 dB. The radiating and receiving devices of the radar units include horizontal magnetic dipoles. The interfaces are separated by comparison of the data of pulse radar detection and ranging of the magnetic field and pulse radar detection and ranging of the electric field.
EFFECT: remote determination of interfaces formed by inversions of the geomagnetic field in ice layers, enhanced depth of survey.
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