Stephen McCarron
A Plio-Pleistocene sediment wedge on the continental shelf west of central Ireland: The Connemara Fan
McCarron, Stephen; Praeg, Daniel; Ó Cofaigh, Colm; Monteys, Xavier; Thébaudeau, Benjamin; Craven, Kieran; Saqab, Muhammad Mudasar; Cova, Andrea
Authors
Daniel Praeg
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
Xavier Monteys
Benjamin Thébaudeau
Kieran Craven
Muhammad Mudasar Saqab
Andrea Cova
Abstract
Glacigenic sediment fans recording shelf edge deposition from marine-terminating ice sheets have previously been recognised along the NW European continental margin from Svalbard to as far south as Donegal, off north-west Ireland. Here we present evidence of a previously unrecognised partially glacially-fed Plio-Pleistocene sediment wedge on the continental shelf west of central Ireland using 2D and 3D seismic reflection data correlated to a commercial borehole. The ‘Connemara Fan’ covers a shelf area of approximately 9000 km2 in water depths of 125–310 m, extending westwards into the Porcupine Seabight from the Irish Mainland Shelf. The wedge comprises up to 160 m of sediment that culminates in a prominent moraininc ridge at seabed and contains two discordant reflection surfaces (R1 and 2) that subdivide it into three seismic units (SU1–3). Stratigraphic boreholes 27/24-2 and 2A located on the inner shelf show that the lower unit (SU1) is composed of Pliocene marine sediments, while SU2 and 3 comprise glacially influenced facies of Quaternary age. Extracts from a 3D seismic data volume within the central part of the fan show channels within the Pliocene succession, while iceberg scours are observed on the R1 and R2 reflectors. The Connemara Fan is inferred to record sediment supply from central western Ireland, with Quaternary units probably recording at least two glacial advance-retreat cycles with ice sheets repeatedly grounding across the inner (Irish Mainland) shelf. Our findings extend the range of glacially-influenced grounding line depocentres southwards along the NW European continental margin.
Citation
McCarron, S., Praeg, D., Ó Cofaigh, C., Monteys, X., Thébaudeau, B., Craven, K., …Cova, A. (2018). A Plio-Pleistocene sediment wedge on the continental shelf west of central Ireland: The Connemara Fan. Marine Geology, 399, 97-114. https://doi.org/10.1016/j.margeo.2018.02.009
Journal Article Type | Article |
---|---|
Acceptance Date | Feb 21, 2018 |
Online Publication Date | Feb 24, 2018 |
Publication Date | May 1, 2018 |
Deposit Date | Feb 27, 2018 |
Publicly Available Date | Feb 24, 2019 |
Journal | Marine Geology |
Print ISSN | 0025-3227 |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 399 |
Pages | 97-114 |
DOI | https://doi.org/10.1016/j.margeo.2018.02.009 |
Public URL | https://durham-repository.worktribe.com/output/1333894 |
Files
Accepted Journal Article
(14.4 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
© 2018 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
You might also like
The geomorphological record of an ice stream to ice shelf transition in Northeast Greenland
(2023)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search