Glaciolacustrine deposits formed in an ice-dammed tributary valley in the south-central Pyrenees: new evidence for late Pleistocene climate

Sancho, C., Rhodes, E.J. orcid.org/0000-0002-0361-8637, Arenas, C. et al. (4 more authors) (2018) Glaciolacustrine deposits formed in an ice-dammed tributary valley in the south-central Pyrenees: new evidence for late Pleistocene climate. Sedimentary Geology, 366. pp. 47-66. ISSN 0037-0738

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Copyright, Publisher and Additional Information: © 2018 Elsevier. This is an author produced version of a paper subsequently published in Sedimentary Geology. Uploaded in accordance with the publisher's self-archiving policy. Article available under the terms of the CC-BY-NC-ND licence (https://creativecommons.org/licenses/by-nc-nd/4.0/)
Keywords: Glaciolacustrine sediments; Ice-dammed lake; Maximum glacier extent; Marine Isotope Stages 4 and 3; South-central Pyrenees
Dates:
  • Published: April 2018
  • Published (online): 3 February 2018
  • Accepted: 31 January 2018
Institution: The University of Sheffield
Academic Units: The University of Sheffield > Faculty of Social Sciences (Sheffield) > Department of Geography (Sheffield)
Depositing User: Symplectic Sheffield
Date Deposited: 28 Feb 2018 11:09
Last Modified: 03 Feb 2020 01:39
Published Version: https://doi.org/10.1016/j.sedgeo.2018.01.008
Status: Published
Publisher: Elsevier
Refereed: Yes
Identification Number: https://doi.org/10.1016/j.sedgeo.2018.01.008

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