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Record #162058:
- #162058
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MARC recordНекоторые аспекты концептуальной модели внутриледниковых дренажных систем
| Title: | Некоторые аспекты концептуальной модели внутриледниковых дренажных систем |
| Title, transliterated: | Nekotorye aspekty kont︠s︡eptualʹnoĭ modeli vnutrilednikovykh drenazhnykh sistem / B.R. Mavli︠u︡dov. |
| Translated title: | About conceptual model of englacial drainage system. |
| Author(s): | Mavli︠u︡dov, B. R. |
| Date: | 2002. |
| Language: | Russian. |
| In: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (2002.), Vol. 92 (2002) |
| Abstract: | Considers way of conceptual model building of inside drainage system of glaciers, finding that though there is no one common system, branched systems are most frequent. Small glaciers typically have linked cavity drainage systems formed from separate channels and caverns, and these features can also be found in large temperate glaciers. Glacier movement may cause fissures and crevasses to extend from localised crevasse zones. |
| Notes: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 92 :172-179 (2002). English summary and figure caption. |
| Keywords: | 551.32 -- Glaciology. 551.324.86 -- Glacier streams. 556 -- Hydrology. 519.673 -- Modelling. E11 -- Glaciology: glaciohydrology. |
| SPRI record no.: | 162058 |
LDR 01948naa#a2200000#a#4500 001 SPRI-162058 005 20230927025227.0 007 ta 008 230927s2002####xx#a##|##|###|0||#0|rus#d 035 ## ‡aSPRI-162058 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aMavli︠u︡dov, B. R. 242 10 ‡aAbout conceptual model of englacial drainage system.‡yeng 245 10 ‡6880-02‡aNekotorye aspekty kont︠s︡eptualʹnoĭ modeli vnutrilednikovykh drenazhnykh sistem /‡cB.R. Mavli︠u︡dov. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2002. 300 ## ‡ap. 172-179 :‡bdiag., table. 500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 92 :172-179 (2002). 500 ## ‡aEnglish summary and figure caption. 520 3# ‡aConsiders way of conceptual model building of inside drainage system of glaciers, finding that though there is no one common system, branched systems are most frequent. Small glaciers typically have linked cavity drainage systems formed from separate channels and caverns, and these features can also be found in large temperate glaciers. Glacier movement may cause fissures and crevasses to extend from localised crevasse zones. 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 ‡a551.324.86 -- Glacier streams.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 92 (2002) ‡wSPRI-33585 880 1# ‡6100-01/(N‡aМавлюдов, Б. Р. 880 10 ‡6245-02/(N‡aНекоторые аспекты концептуальной модели внутриледниковых дренажных систем /‡cБ.Р. Мавлюдов. 880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 92 (2002) ‡wSPRI-33585 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230927