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Record #162058:

Некоторые 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

MARCXML

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005 20221001101609.0
007 ta
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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# ‡a20221001