Четвертичное оледенение в горах Сибири как результат взаимодействия гляциальных и мерзлотных процессов

MARCXML

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001 SPRI-189373
005 20240418015738.0
007 ta
008 240418s2008####xx#ab#|##|###|0||#0|rus#d
035 ## ‡aSPRI-189373
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aSheĭnkman, V. S.
242 10 ‡aQuaternary glaciaiton in the Siberian mountains as a result of glacial and permafrost processes interaction.‡yeng
245 10 ‡6880-02‡aChetvertichnoe oledenenie v gorakh Sibiri kak rezulʹtat vzaimodeĭstvii︠a︡ gli︠a︡t︠s︡ialʹnykh i merzlotnykh prot︠s︡essov /‡cV.S. Sheĭnkman.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2008.
300 ## ‡ap. 51-72 :‡bill., maps.
500 ## ‡aMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. Vol. 105 :51-72 (2008).
500 ## ‡aEnglish summary and captions.
520 3# ‡aExamines glaciation specificity in mountains of Siberia in relation to glacio- and cryogenesis. Analyzes glacial environments and possible development scenarios, arguing that glaciation has been mainly mountain in character, becoming reticular under most suitable conditions of Late Pleistocene. Environments have been characterized by interaction of cryogenic and glacier ice, with cryoaridization determining environmental cooling against background of increasing climate continentality. Glaciers have generally experienced low snow accumulation, relying on cold storage and supply from superimposed ice. Finds no evidence of ancient glaciations, but good correlation between cold units in palaeoclimate records and cryogenic epochs. Views glaciation in Siberian mountains as process superimposed upon and supplementing cryogenesis.
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 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.43 -- Reconstruction of ancient relief.‡2udc
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.582 -- Climatology of particular places.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.343.74 -- Naleds. Icings. Aufeis.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc
650 07 ‡a551.324.6 -- Land ice, fluctuation.‡2udc
650 07 ‡a551.324.431 -- Land ice, accumulation.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*501) -- Russia (Federation).‡2udc
651 #7 ‡a(*501.3) -- East Siberia.‡2udc
773 0# ‡6880-03‡7nnas ‡tMaterialy Gli︠a︡t︠s︡iologicheskikh Issledovaniĭ. ‡gVol. 105 (2008) ‡wSPRI-33585
880 1# ‡6100-01/(N‡aШейнкман, В. С.
880 10 ‡6245-02/(N‡aЧетвертичное оледенение в горах Сибири как результат взаимодействия гляциальных и мерзлотных процессов /‡cВ.С. Шейнкман.
880 0# ‡6773-03/(N‡7nnas ‡tМатериалы Гляциологических Исследований. ‡gVol. 105 (2008) ‡wSPRI-33585
916 ## ‡a2010/01/21 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240418 ‡bRF