Infill of tunnel valleys associated with landward‐flowing ice sheets: The missing Middle Pleistocene record of the NW European rivers?

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Standard

Infill of tunnel valleys associated with landward‐flowing ice sheets : The missing Middle Pleistocene record of the NW European rivers? / Moreau, Julien; Huuse, Mads.

I: Geochemistry, Geophysics, Geosystems, Bind 15, Nr. 1, 01.2014, s. 1-9.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Moreau, J & Huuse, M 2014, 'Infill of tunnel valleys associated with landward‐flowing ice sheets: The missing Middle Pleistocene record of the NW European rivers?', Geochemistry, Geophysics, Geosystems, bind 15, nr. 1, s. 1-9. https://doi.org/10.1002/2013GC005007

APA

Moreau, J., & Huuse, M. (2014). Infill of tunnel valleys associated with landward‐flowing ice sheets: The missing Middle Pleistocene record of the NW European rivers? Geochemistry, Geophysics, Geosystems, 15(1), 1-9. https://doi.org/10.1002/2013GC005007

Vancouver

Moreau J, Huuse M. Infill of tunnel valleys associated with landward‐flowing ice sheets: The missing Middle Pleistocene record of the NW European rivers? Geochemistry, Geophysics, Geosystems. 2014 jan.;15(1):1-9. https://doi.org/10.1002/2013GC005007

Author

Moreau, Julien ; Huuse, Mads. / Infill of tunnel valleys associated with landward‐flowing ice sheets : The missing Middle Pleistocene record of the NW European rivers?. I: Geochemistry, Geophysics, Geosystems. 2014 ; Bind 15, Nr. 1. s. 1-9.

Bibtex

@article{5c5f8a11478a48358c7bf6abef76b256,
title = "Infill of tunnel valleys associated with landward‐flowing ice sheets: The missing Middle Pleistocene record of the NW European rivers?",
abstract = "The southern termination of the Middle and Late Pleistocene Scandinavian ice sheets was repeatedly located in the southern North Sea (sNS) and adjacent, north-sloping land areas. Giant meltwater-excavated valleys (tunnel valleys) formed at the southern termination of the ice sheets and contain a hitherto enigmatic succession of northward prograding clinoforms, comprising 1000s km 3 of sediment. This study analyses 3D seismic data, covering the entire sNS, and demonstrates for the first time that the formation of these tunnel valleys was separate from their infill. The infill constitutes the postglacial record of the NW European river deltas, which had so far been considered missing.",
author = "Julien Moreau and Mads Huuse",
year = "2014",
month = jan,
doi = "10.1002/2013GC005007",
language = "English",
volume = "15",
pages = "1--9",
journal = "Geochemistry, Geophysics, Geosystems",
issn = "1525-2027",
publisher = "AGU Publications",
number = "1",

}

RIS

TY - JOUR

T1 - Infill of tunnel valleys associated with landward‐flowing ice sheets

T2 - The missing Middle Pleistocene record of the NW European rivers?

AU - Moreau, Julien

AU - Huuse, Mads

PY - 2014/1

Y1 - 2014/1

N2 - The southern termination of the Middle and Late Pleistocene Scandinavian ice sheets was repeatedly located in the southern North Sea (sNS) and adjacent, north-sloping land areas. Giant meltwater-excavated valleys (tunnel valleys) formed at the southern termination of the ice sheets and contain a hitherto enigmatic succession of northward prograding clinoforms, comprising 1000s km 3 of sediment. This study analyses 3D seismic data, covering the entire sNS, and demonstrates for the first time that the formation of these tunnel valleys was separate from their infill. The infill constitutes the postglacial record of the NW European river deltas, which had so far been considered missing.

AB - The southern termination of the Middle and Late Pleistocene Scandinavian ice sheets was repeatedly located in the southern North Sea (sNS) and adjacent, north-sloping land areas. Giant meltwater-excavated valleys (tunnel valleys) formed at the southern termination of the ice sheets and contain a hitherto enigmatic succession of northward prograding clinoforms, comprising 1000s km 3 of sediment. This study analyses 3D seismic data, covering the entire sNS, and demonstrates for the first time that the formation of these tunnel valleys was separate from their infill. The infill constitutes the postglacial record of the NW European river deltas, which had so far been considered missing.

U2 - 10.1002/2013GC005007

DO - 10.1002/2013GC005007

M3 - Journal article

VL - 15

SP - 1

EP - 9

JO - Geochemistry, Geophysics, Geosystems

JF - Geochemistry, Geophysics, Geosystems

SN - 1525-2027

IS - 1

ER -

ID: 100050043