Structure, Distribution and Formation of Submarine Permafrost (Osobennosti Stroeniia, Rasprostraneniia i Formirovaniia Subakval'noi Kriogenno i Tolshchi)

This research conducted in the eastern part of the Laptev Sea has once again confirmed the extremely complex nature of the subaquatic cryozenic stratum, which is expressed by the instability and dynamicity of this layer. The thermal state and structure of submarine permafrost, the thermodynamic aspe...

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Bibliographic Details
Main Authors: Zhigarev,L. A., Piakht,I. R.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1976
Subjects:
Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
*CONTINENTAL SHELVES
*STRUCTURAL GEOLOGY
*PERMAFROST
USSR
THICKNESS
DISTRIBUTION
THERMODYNAMICS
STRATIGRAPHY
MARINE GEOLOGY
SEASONAL VARIATIONS
TRANSLATIONS
INSTABILITY
SEA ICE
*Laptev sea(USSR)
Laptev Sea
Ice
laptev
permafrost
Sea ice
Online Access:http://www.dtic.mil/docs/citations/ADA024555
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA024555
Description
Summary:This research conducted in the eastern part of the Laptev Sea has once again confirmed the extremely complex nature of the subaquatic cryozenic stratum, which is expressed by the instability and dynamicity of this layer. The thermal state and structure of submarine permafrost, the thermodynamic aspects of the conditions for the formation, preservation and destruction of cryozenic formations on the shelf are discussed. (Author) Draft trans. of mono. Problems of Cryolithology (USSR) 1974 p115-124.

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