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Record #114060:
- #114060
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MARC recordОсобенности пространственного строения глубинного льда в районе станции Восток, Антарктида
| Title: | Особенности пространственного строения глубинного льда в районе станции Восток, Антарктида |
| Title, transliterated: | Osobennosti prostranstvennogo stroenii︠a︡ glubinnogo lʹda v raĭone stant︠s︡ii Vostok, Antarktida / I︠U︡.M. Chashchinov, A.E. Rakhmanov. |
| Translated title: | Peculiarities of the spatial structure of depth ice in the area of Vostok station, Antarctica. |
| Author(s): | Chashchinov, I︠U︡. M. Rakhmanov, A. E. |
| Date: | 1991. |
| Language: | Russian. |
| In: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (1991.), Vol. 71 (1991) |
| Abstract: | Investigation of orientation of grains in ice from Vostok. Concludes that both plastic deformation and recrystallization occur between 0 and 650 m depth, while plastic deformation dominates at greater depths. |
| Notes: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 71 :121-125 (1991). English summary p. 125. |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.24 -- Ice sheets and caps. 548.53 -- Ice, recrystallization and grain growth. 548.2 -- Ice, granular structure. Anisotropy. 539.37 -- Ice, plastic and viscous deformation. 551.324.8 -- Land ice, structure and surface features. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*74) -- Australian Antarctic Territory. (*747.5) -- Vostok region. |
| SPRI record no.: | 114060 |
LDR 02245naa#a2200000#a#4500 001 SPRI-114060 005 20240416154323.0 007 ta 008 240416s1991####xx#a##|##|###|0||#0|rus#d 035 ## ‡aSPRI-114060 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aChashchinov, I︠U︡. M. 242 10 ‡aPeculiarities of the spatial structure of depth ice in the area of Vostok station, Antarctica.‡yeng 245 10 ‡6880-02‡aOsobennosti prostranstvennogo stroenii︠a︡ glubinnogo lʹda v raĭone stant︠s︡ii Vostok, Antarktida /‡cI︠U︡.M. Chashchinov, A.E. Rakhmanov. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 121-125 :‡bdiags. 500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 71 :121-125 (1991). 500 ## ‡aEnglish summary p. 125. 520 3# ‡aInvestigation of orientation of grains in ice from Vostok. Concludes that both plastic deformation and recrystallization occur between 0 and 650 m depth, while plastic deformation dominates at greater depths. 546 ## ‡aIn Russian. 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 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc 650 07 ‡a548.53 -- Ice, recrystallization and grain growth.‡2udc 650 07 ‡a548.2 -- Ice, granular structure. Anisotropy.‡2udc 650 07 ‡a539.37 -- Ice, plastic and viscous deformation.‡2udc 650 07 ‡a551.324.8 -- Land ice, structure and surface features.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*74) -- Australian Antarctic Territory.‡2udc 651 #7 ‡a(*747.5) -- Vostok region.‡2udc 700 1# ‡6880-03‡aRakhmanov, A. E. 773 0# ‡6880-04‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 71 (1991) ‡wSPRI-33585 880 1# ‡6100-01/(N‡aЧащинов, Ю. М. 880 10 ‡6245-02/(N‡aОсобенности пространственного строения глубинного льда в районе станции Восток, Антарктида /‡cЮ.М. Чащинов, А.Е. Рахманов. 880 1# ‡6700-03/(N‡aРахманов, А. Е. 880 0# ‡6773-04/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 71 (1991) ‡wSPRI-33585 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416