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Permafrost as the main factor controlling the fluvial sedimentation style on glaciomarginal fans

cris.lastimport.scopus2024-02-12T20:39:36Z
dc.abstract.enThis study describes the sedimentary successions of two glaciomarginal fans (=end moraines) deposited during MIS 6 and MIS 2 in the eastern and north-western part of Poland. Sedimentological analyses of the successions in- dicate they were both deposited close to the ice sheet margin and are dominated by extensive gravelly and sandy sheet beds derivedfrom the upperflow regimewithsingle ice-wedge structures.Qualitativeand quantitativeanal- ysisof the pancake-like gravelly and sandy sediments wa s performed using Markov chain analysis. The presence of these, admittedly common, sedimentary successions raises two key points: why sheetfloods are so common on glaciomarginal fans instead of in-channel flows, and whether sedimentary rhythms deposited by sheetfloods rep- resent the full depositional records, or only partial ones due to accompanying erosion. While both points remain unclear, the answers to these questions may be connected to the presence of permafrost, which occupied the fore- land of the ice sheet where the glaciomarginal fans were deposited: it can control the type of proglacial river flows on glaciomarginal fans, the depth of erosion and influence the record of sedimentary rhythms.
dc.affiliationUniwersytet Warszawski
dc.contributor.authorBujak, Łukasz
dc.contributor.authorPisarska-Jamroży, Małgorzata
dc.contributor.authorWoronko, Barbara
dc.contributor.authorMleczak, Mateusz
dc.date.accessioned2024-01-25T16:35:04Z
dc.date.available2024-01-25T16:35:04Z
dc.date.issued2021
dc.description.financePublikacja bezkosztowa
dc.description.volume422
dc.identifier.doi10.1016/J.SEDGEO.2021.105971
dc.identifier.issn0037-0738
dc.identifier.urihttps://repozytorium.uw.edu.pl//handle/item/115721
dc.identifier.weblinkhttps://doi.org/10.1016/j.sedgeo.2021.105971
dc.languageeng
dc.pbn.affiliationearth and related environmental sciences
dc.relation.ispartofSedimentary Geology
dc.relation.pages1-16
dc.rightsClosedAccess
dc.sciencecloudnosend
dc.subject.enGlaciomarginal fan
dc.subject.enPermafrost
dc.subject.enPleistocene
dc.subject.enMarkov chain analysis
dc.subject.enSheetflood/sheetflow
dc.titlePermafrost as the main factor controlling the fluvial sedimentation style on glaciomarginal fans
dc.typeJournalArticle
dspace.entity.typePublication