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Record #114050:
Эрозионно-аккумулятивная деятельность ледников северного Тянь-Шаня в малом ледниковом периоде
Title: | Эрозионно-аккумулятивная деятельность ледников северного Тянь-Шаня в малом ледниковом периоде |
Title, transliterated: | Ėrozionno-akkumuli︠a︡tivnai︠a︡ dei︠a︡telʹnostʹ lednikov severnogo Ti︠a︡nʹ-Shani︠a︡ v malom lednikovom periode / A.V. Orlov. |
Translated title: | Erosive-accumulative activity of glaciers of northern Tyan'-Shan' in the Little Ice Age. |
Author(s): | Orlov, A. V. |
Date: | 1991. |
Language: | Russian. |
In: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. (1991.), Vol. 71 (1991) |
Abstract: | Discusses precise criteria for separation of super- and subglacial debris. Analysis of composition of subglacial debris made it possible to identify zone of maximum exaration of basal rock and to reconstruct dynamics during Little Ice Age, related to significant changes in extent of glaciers during advance and retreat. Concentration of subglacial debris occurs at margins of glacier under actively moving ice. Disintegration of debris fragments is caused mainly by processes of milling and abrasion. |
Notes: | Materialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 71 :59-65 (1991). English summary p. 65. |
Keywords: | 551.33 -- Glacial geology. 551.331.4 -- Glacial erosion, processes. 551.331.5 -- Glacial erosion and protection. Sub-glacial topography. 551.332.51 -- Ice-marginal landforms. E7 -- Glaciology: glacial geology and ice ages. (235.21) -- Hindu Kush and Tien Shan. |
SPRI record no.: | 114050 |
LDR 02210naa#a2200000#a#4500 001 SPRI-114050 005 20240328223931.0 007 ta 008 240328s1991####xx#a##|##|###|0||#0|rus#d 035 ## ‡aSPRI-114050 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aOrlov, A. V. 242 10 ‡aErosive-accumulative activity of glaciers of northern Tyan'-Shan' in the Little Ice Age.‡yeng 245 10 ‡6880-02‡aĖrozionno-akkumuli︠a︡tivnai︠a︡ dei︠a︡telʹnostʹ lednikov severnogo Ti︠a︡nʹ-Shani︠a︡ v malom lednikovom periode /‡cA.V. Orlov. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 59-65 :‡bdiags. 500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 71 :59-65 (1991). 500 ## ‡aEnglish summary p. 65. 520 3# ‡aDiscusses precise criteria for separation of super- and subglacial debris. Analysis of composition of subglacial debris made it possible to identify zone of maximum exaration of basal rock and to reconstruct dynamics during Little Ice Age, related to significant changes in extent of glaciers during advance and retreat. Concentration of subglacial debris occurs at margins of glacier under actively moving ice. Disintegration of debris fragments is caused mainly by processes of milling and abrasion. 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 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.331.4 -- Glacial erosion, processes.‡2udc 650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc 650 07 ‡a551.332.51 -- Ice-marginal landforms.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(235.21) -- Hindu Kush and Tien Shan.‡2udc 773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 71 (1991) ‡wSPRI-33585 880 1# ‡6100-01/(N‡aОрлов, А. В. 880 10 ‡6245-02/(N‡aЭрозионно-аккумулятивная деятельность ледников северного Тянь-Шаня в малом ледниковом периоде /‡cА.В. Орлов. 880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 71 (1991) ‡wSPRI-33585 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328