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We present the results of the use of the Ground Penetrating Radar (GPR) method on saline and nonsaline soils in permafrost rock zones. GPR records are geologically interpreted during thermokarst and pingo study. The usefulness of the GPR method for mapping the top and bottom of permafrost rocks is explored for saline soils.
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Ermakov et al. (2010) studied this question.
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