1887

Abstract

Gravity and magnetic profile measurements and EM-frequency soundings were carried out on a 0 - 1000 m thick glacier between nunataks. Information on ice thickness, its conductivity and bedrock variations under glacier was obtained. A wide conductor, which is interpreted to be saltwater enriched below permafrost, was revealed.

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/content/papers/10.3997/2214-4609.201409425
1995-05-29
2021-06-18
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409425
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