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1000 Titel
  • Extensive palaeo-surfaces beneath the Evans–Rutford region of the West Antarctic Ice Sheet control modern and past ice flow
1000 Autor/in
  1. Carter, Charlotte M. |
  2. Bentley, Michael J. |
  3. Jamieson, Stewart S. R. |
  4. Paxman, Guy J. G. |
  5. Jordan, Tom A. |
  6. Bodart, Julien A. |
  7. Ross, Neil |
  8. Napoleoni, Felipe |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-07
1000 Erschienen in
1000 Quellenangabe
  • 18(5):2277-2296
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-2277-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The subglacial landscape of Antarctica records and influences the behaviour of its overlying ice sheet. However, in many places, the evolution of the landscape and its control on ice sheet behaviour have not been investigated in detail. Using recently released radio-echo sounding data, we investigate the subglacial landscape of the Evans–Rutford region of West Antarctica. Following quantitative analysis of the landscape morphology under ice-loaded and ice-unloaded conditions, we identify 10 flat surfaces distributed across the region. Across these 10 surfaces, we identify two distinct populations based on clustering of elevations, which potentially represent remnants of regionally coherent pre-glacial surfaces underlying the West Antarctic Ice Sheet (WAIS). The surfaces are bounded by deeply incised glacial troughs, some of which have potential tectonic controls. We assess two hypotheses for the evolution of the regional landscape: (1) passive-margin evolution associated with the break-up of the Gondwana supercontinent or (2) an extensive planation surface that may have been uplifted in association with either the West Antarctic Rift System or cessation of subduction at the base of the Antarctic Peninsula. We suggest that passive-margin evolution is the most likely of these two mechanisms, with the erosion of glacial troughs adjacent to, and incising, the flat surfaces likely having coincided with the growth of the WAIS. These flat surfaces also demonstrate similarities to other identified surfaces, indicating that a similar formational process may have been acting more widely around the Weddell Sea embayment. The subsequent fluctuations of ice flow, basal thermal regime, and erosion patterns of the WAIS are therefore controlled by the regional tectonic structures. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/Q2FydGVyLCBDaGFybG90dGXCoE0u|https://frl.publisso.de/adhoc/uri/QmVudGxleSwgTWljaGFlbMKgSi4=|https://frl.publisso.de/adhoc/uri/SmFtaWVzb24sIFN0ZXdhcnTCoFMuwqBSLg==|https://frl.publisso.de/adhoc/uri/UGF4bWFuLCBHdXnCoEouwqBHLg==|https://frl.publisso.de/adhoc/uri/Sm9yZGFuLCBUb23CoEEu|https://frl.publisso.de/adhoc/uri/Qm9kYXJ0LCBKdWxpZW7CoEEu|https://frl.publisso.de/adhoc/uri/Um9zcywgTmVpbA==|https://frl.publisso.de/adhoc/uri/TmFwb2xlb25pLCBGZWxpcGU=
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1000 Label
1000 Förderer
  1. Natural Environment Research Council |
  2. H2020 European Research Council |
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1000 Dateien
1000 Förderung
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    1000 Förderer Natural Environment Research Council |
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    1000 Fördernummer -
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    1000 Förderer H2020 European Research Council |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6482029.rdf
1000 Erstellt am 2024-05-24T02:14:21.545+0200
1000 Erstellt von 322
1000 beschreibt frl:6482029
1000 Zuletzt bearbeitet Mon May 27 14:05:25 CEST 2024
1000 Objekt bearb. Mon May 27 14:05:25 CEST 2024
1000 Vgl. frl:6482029
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