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Record #88394:

Peculiarities of the morphology of glacial dislocations on the Kara Sea coast / V.M. Smirnov.

Title: Peculiarities of the morphology of glacial dislocations on the Kara Sea coast / V.M. Smirnov.
Author(s): Smirnov, V. M.
Date: 1987.
Language: Russian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
In: Polar Geography and Geology. (1987.), Vol. 11(4) (1987)
Abstract: Description of tight, asymmetrical minor folds in well-bedded sands, loams and clays exposed by thermal abrasion of ice-rich sediments on west coast of Yamal and north coast of Yugorskiy Poluostrov. Folds are commonly underlain by massive bodies of ground ice, and may be product of southward flow of ice within ice sheet sitting on Kara shelf, over unconsolidated sediments which were already frozen. Translated from Akademiya Nauk SSSR. Izvestiya. Seriya Geograficheskaya, 1987, No.3, p.103-107.
Notes:

Polar Geography and Geology. Vol. 11(4) :273-278 (1987).

Keywords: 551.333 -- Glacial deformation and glaciotectonic structures.
551.345.3 -- Permafrost, composition and structure. Ice wedges.
E8 -- Glaciology: frost action and permafrost.
(*50) -- Soviet Union.
(*531.51) -- Yamalo-Nenetskiy Avtonomnyy Okrug.
(*531.71) -- Nenetskiy Avtonomnyy Okrug.
SPRI record no.: 88394

MARCXML

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005 20230326002209.0
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035 ## ‡aSPRI-88394
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100 1# ‡aSmirnov, V. M.
240 10 ‡6880-01‡aOsobennosti morfologii gli︠a︡t︠s︡iodislokat︠s︡iĭ na poberezhʹe Karskogo mori︠a︡.‡lRussian
245 10 ‡aPeculiarities of the morphology of glacial dislocations on the Kara Sea coast /‡cV.M. Smirnov.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1987.
300 ## ‡ap. 273-278 :‡bill., map.
500 ## ‡aPolar Geography and Geology. Vol. 11(4) :273-278 (1987).
520 3# ‡aDescription of tight, asymmetrical minor folds in well-bedded sands, loams and clays exposed by thermal abrasion of ice-rich sediments on west coast of Yamal and north coast of Yugorskiy Poluostrov. Folds are commonly underlain by massive bodies of ground ice, and may be product of southward flow of ice within ice sheet sitting on Kara shelf, over unconsolidated sediments which were already frozen. Translated from Akademiya Nauk SSSR. Izvestiya. Seriya Geograficheskaya, 1987, No.3, p.103-107.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a551.333 -- Glacial deformation and glaciotectonic structures.‡2udc
650 07 ‡a551.345.3 -- Permafrost, composition and structure. Ice wedges.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*50) -- Soviet Union.‡2udc
651 #7 ‡a(*531.51) -- Yamalo-Nenetskiy Avtonomnyy Okrug.‡2udc
651 #7 ‡a(*531.71) -- Nenetskiy Avtonomnyy Okrug.‡2udc
773 0# ‡7nnas ‡tPolar Geography and Geology. ‡gVol. 11(4) (1987) ‡wSPRI-56066
880 10 ‡6240-01/(N‡aОсобенности морфологии гляциодислокаций на побережье Карского моря.‡lRussian
917 ## ‡aUnenhanced record from Muscat, imported 2019
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