Depositional history of the North Taymyr ice-marginal zone, Siberia - a landsystem approach

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Fältnamn	Indikatorer	Metadata
000		03587naa a2200421 4500
001		oai:lup.lub.lu.se:188dfd8f-7803-40dd-a736-454c2b141a0b
003		SwePub
008		160401s2002 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://lup.lub.lu.se/record/3322672 URI
024	7	a https://doi.org/10.1002/jqs.6772 DOI
040		a (SwePub)lu
041		a engb eng
042		9 SwePub
072	7	a art2 swepub-publicationtype
072	7	a ref2 swepub-contenttype
100	1	a Alexanderson, Helenau Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-hal
245	1 0	a Depositional history of the North Taymyr ice-marginal zone, Siberia - a landsystem approach
264		c 2002-05-30
264	1	b Wiley,c 2002
520		a The sediment-landform associations of the northern Taymyr Peninsula in Arctic Siberia tell a tale of ice sheets advancing from the Kara Sea shelf and inundating the peninsula, probably three times during the Weichselian. In each case the ice sheet had a margin frozen to its bed and an interior moving over a deforming bed. The North Taymyr ice-marginal zone (NTZ) comprises ice-marginal and supraglacial landsystems dominated by thrust-block moraines 2-3 km wide and large-scale deformation of sediments and ice. Large areas are still underlain by remnant glacier ice and a supraglacial landscape with numerous ice-walled lakes and kames is forming even today. The proglacial landsystem is characterised by subaqueous (e.g. deltas) or terrestrial (e.g. sandar) environments, depending on location/altitude and time of formation. Dating results (OSL, C-14) indicate that the NTZ was initiated ca. 80 kyr BP during the retreat of the Early Weichselian ice sheet and that it records the maximum limit of a Middle Weichselian glaciation (ca. 65 kyr BP). During both these events, proglacial lakes were dammed by the ice sheets. Part of the NTZ was occupied by a thin Late Weichselian ice sheet (20-12 kyr BP), resulting in subaerial proglacial drainage. Copyright (C) 2002 John Wiley Sons, Ltd.
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
653		a glaciation
653		a ice-marginal zone
653		a landsystem
653		a Weichselian
653		a Siberia
700	1	a Adrielsson, Lenau Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-lad
700	1	a Hjort, Christianu Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-chj
700	1	a Möller, Peru Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science4 aut0 (Swepub:lu)geol-pmo
700	1	a Antonov, O4 aut
700	1	a Eriksson, S4 aut
700	1	a Pavlov, M4 aut
710	2	a Kvartärgeologib Geologiska institutionen4 org
773	0	t Journal of Quaternary Scienced : Wileyg 17:4, s. 361-382q 17:4<361-382x 1099-1417x 0267-8179
856	4	u http://dx.doi.org/10.1002/jqs.677y FULLTEXT
856	4 8	u https://lup.lub.lu.se/record/332267
856	4 8	u https://doi.org/10.1002/jqs.677

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Av författaren/redakt...: Alexanderson, He ...; Adrielsson, Lena; Hjort, Christian; Möller, Per; Antonov, O; Eriksson, S; visa fler...; Pavlov, M; visa färre...

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