REMOTE SENSING DETERMINATION OF BOUNDARIES IN ICE SHEETS FORMED BY GEOMAGNETIC FIELD REVERSALS

Abstract

Considered is the possibility of remote, upon motion from the Earth as well as air, detecting, isolating and determining the bedding depth of boundaries in magnetization formed in polar glacier ice strata by geomagnetic field reversals, using correlating of results of radiolocation probing with magnetic and electric pulses. It enables to investigate the glacier development dynamics in time and space. The investigation depth is sufficient for studying the whole ice strata of any polar glaciers.