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Record #117892:
The origin of the ground ice in the Malyk-Sien basin, northeastern USSR / V.V. Zamoruyev.
Title: | The origin of the ground ice in the Malyk-Sien basin, northeastern USSR / V.V. Zamoruyev. |
Author(s): | Zamoruyev, V. V. |
Date: | 1992. |
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. (1992.), Vol. 16(1) (1992) |
Abstract: | Quaternary sequence in basin includes beds of diamicton sediments and ground-ice bodies. Up to now, latter have been considered to be fossil glacier ice and former to be till. However, re-examination suggests that ground ice represents bodies of accumulative ice, ice wedges, buried river ice, and icings (aufeis) |
Notes: | Polar Geography and Geology. Vol. 16(1) :65-71 (1992). Translation of article in Materialy Glyatsiologicheskiy Issledovaniy, No. 71, 1991, p. 149-153. |
Keywords: | 551.34 -- Geocryology. Frozen ground. 551.345 -- Permafrost. Cryopedology. 551.345.3 -- Permafrost, composition and structure. Ice wedges. 551.343.74 -- Naleds. Icings. Aufeis. E8 -- Glaciology: frost action and permafrost. (*501) -- Russia (Federation). |
SPRI record no.: | 117892 |
LDR 01814naa#a2200000#a#4500 001 SPRI-117892 005 20230607135758.0 007 ta 008 230607s1992####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-117892 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aZamoruyev, V. V. 240 10 ‡6880-01‡aO proiskhozhdenii podzemnykh lʹdov Malyk-Siėnskoĭ vpadiny, Severo-Vostok SSSR.‡lRussian 245 14 ‡aThe origin of the ground ice in the Malyk-Sien basin, northeastern USSR /‡cV.V. Zamoruyev. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 65-71 :‡bdiags. 500 ## ‡aPolar Geography and Geology. Vol. 16(1) :65-71 (1992). 500 ## ‡aTranslation of article in Materialy Glyatsiologicheskiy Issledovaniy, No. 71, 1991, p. 149-153. 520 3# ‡aQuaternary sequence in basin includes beds of diamicton sediments and ground-ice bodies. Up to now, latter have been considered to be fossil glacier ice and former to be till. However, re-examination suggests that ground ice represents bodies of accumulative ice, ice wedges, buried river ice, and icings (aufeis) 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 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a551.345.3 -- Permafrost, composition and structure. Ice wedges.‡2udc 650 07 ‡a551.343.74 -- Naleds. Icings. Aufeis.‡2udc 650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local 651 #7 ‡a(*501) -- Russia (Federation).‡2udc 773 0# ‡7nnas ‡tPolar Geography and Geology. ‡gVol. 16(1) (1992) ‡wSPRI-56066 880 10 ‡6240-01/(N‡aО происхождении подземных льдов Малык-Сиэнской впадины, Северо-Восток СССР.‡lRussian 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230607