The provenance of the Devonian Old Red Sandstone of the Dingle Peninsula, SW Ireland; the earliest record of Laurentian and peri-Gondwanan sediment mixing in Ireland

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dc.contributor.author Fairey, Brenton J.
dc.contributor.author Kerrison, Aidan
dc.contributor.author Meere, Patrick A.
dc.contributor.author Mulchrone, Kieran F.
dc.contributor.author Hofmann, Mandy
dc.contributor.author Gärtner, Andreas
dc.contributor.author Sonntag, Benita-Lisette
dc.contributor.author Linnemann, Ulf
dc.contributor.author Kuiper, Klaudia F.
dc.contributor.author Ennis, Meg
dc.contributor.author Mark, Chris
dc.contributor.author Cogné, Nathan
dc.contributor.author Chew, David
dc.date.accessioned 2018-07-24T09:13:14Z
dc.date.available 2018-07-24T09:13:14Z
dc.date.issued 2018-01-17
dc.identifier.citation Fairey, B. J., Kerrison, A., Meere, P. A., Mulchrone, K. F., Hofmann, M., Gärtner, A., Sonntag, B.-L., Linnemann, U., Kuiper, K. F., Ennis, M., Mark, C., Cogné, N. and Chew, D. (2018) 'The provenance of the Devonian Old Red Sandstone of the Dingle Peninsula, SW Ireland; the earliest record of Laurentian and peri-Gondwanan sediment mixing in Ireland', Journal of the Geological Society, 175(3), pp. 411-424. doi:10.1144/jgs2017-099 en
dc.identifier.volume 175 en
dc.identifier.issued 3 en
dc.identifier.startpage 411 en
dc.identifier.endpage 424 en
dc.identifier.issn 0016-7649
dc.identifier.issn 2041-479X
dc.identifier.uri http://hdl.handle.net/10468/6494
dc.identifier.doi 10.1144/jgs2017-099
dc.description.abstract The Lower Old Red Sandstone in southern Ireland is hosted in the Early Devonian Dingle Basin, which lies immediately south of the Iapetus Suture on the Dingle Peninsula, County Kerry. The basin developed as a post-Caledonian pullapart structure prior to Acadian deformation, which in turn was followed by end-Carboniferous Variscan deformation. Detrital zircon U–Th–Pb geochronology is complemented by mica Ar–Ar and apatite U–Pb geochronology to gain a comprehensive understanding of the provenance of the Lower Devonian Lower Old Red Sandstone of the Dingle Basin and assess contributions of major tectonic components (e.g. Laurentia, Ganderia). Sedimentary rocks in the Lower Old Red Sandstone have similar detrital zircon age distributions, which are dominated by c. 1.2 Ga zircons as well as late Neoproterozoic grains. This indicates a dominant contribution of detritus of Laurentian affinity as well as contributions from westerly and southerly derived Ganderian detritus. Caledonian uplift of the area north of the Iapetus Suture would have facilitated a large contribution of (peri-)Laurentian material. The Upper Old Red Sandstone on the Dingle Peninsula has a distinctly different detrital zircon character including few late Neoproterozoic zircons and abundant zircons of c. 1.05 Ga age, indicating sediment derivation only from Laurentia and no recycling from the Lower Old Red Sandstone. en
dc.description.sponsorship Irish Petroleum Infrastructure Programme (Irish Shelf Petroleum Studies Group 4 (Project Code IS 12/05 UCC); Nederlandse Organisatie voor Wetenschappelijk Onderzoek (Grant 864.12.005) en
dc.format.mimetype application/pdf en
dc.language.iso en en
dc.publisher The Geological Society of London en
dc.relation.uri https://doi.org/10.6084/m9.figshare.c.3971862
dc.rights © 2018, the Authors. Published by The Geological Society of London. All rights reserved. This document is the Accepted Manuscript version of a Published Work that appeared in final form in Journal of the Geological Society. To access the final edited and published work see https://doi.org/10.1144/jgs2017-099 en
dc.subject Laurentia en
dc.subject Ganderia en
dc.subject 1.2 Ga zircons en
dc.subject Late Neoproterozoic grains en
dc.subject Caledonian uplift en
dc.subject Sediment derivation en
dc.title The provenance of the Devonian Old Red Sandstone of the Dingle Peninsula, SW Ireland; the earliest record of Laurentian and peri-Gondwanan sediment mixing in Ireland en
dc.type Article (peer-reviewed) en
dc.internal.authorcontactother Kieran Mulchrone, School Of Mathematical Sciences, University College Cork, Cork, Ireland. +353-21-490-3000 Email: k.mulchrone@ucc.ie en
dc.internal.availability Full text available en
dc.check.info Access to this article is restricted until 12 months after publication by request of the publisher. en
dc.check.date 2019-01-17
dc.date.updated 2018-07-24T08:44:25Z
dc.description.version Accepted Version en
dc.internal.rssid 446854252
dc.contributor.funder Science Foundation Ireland en
dc.contributor.funder European Regional Development Fund en
dc.contributor.funder Nederlandse Organisatie voor Wetenschappelijk Onderzoek en
dc.contributor.funder Petroleum Infrastructure Programme, Ireland
dc.description.status Peer reviewed en
dc.identifier.journaltitle Journal of the Geological Society en
dc.internal.copyrightchecked Yes en
dc.internal.licenseacceptance Yes en
dc.internal.IRISemailaddress k.mulchrone@ucc.ie en
dc.relation.project info:eu-repo/grantAgreement/SFI/SFI Investigator Programme/12/IP/1663/IE/Microanalysis of detrital apatite: a new provenance proxy in sedimentary systems/ en
dc.relation.project info:eu-repo/grantAgreement/SFI/SFI Research Centres/13/RC/2092/IE/Irish Centre for Research in Applied Geosciences (iCRAG)/ en


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