Prelithification and synlithification tectonic foliation development in a clastic sedimentary sequence

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dc.contributor.author Meere, Patrick A.
dc.contributor.author Mulchrone, Kieran F.
dc.contributor.author McCarthy, David J.
dc.contributor.author Timmerman, Martin J.
dc.contributor.author Dewey, John F.
dc.date.accessioned 2018-05-31T15:26:33Z
dc.date.available 2018-05-31T15:26:33Z
dc.date.issued 2016-04
dc.identifier.citation Meere, P. A., Mulchrone, K. F., McCarthy, D. J., Timmerman, M. J. and Dewey, J. F. (2016) 'Prelithification and synlithification tectonic foliation development in a clastic sedimentary sequence', (2016) Geology, 44(4), pp. 291-294. doi:10.1130/G37587.1 en
dc.identifier.volume 44 en
dc.identifier.issued 4 en
dc.identifier.startpage 291 en
dc.identifier.endpage 294 en
dc.identifier.issn 0091-7613
dc.identifier.uri http://hdl.handle.net/10468/6240
dc.identifier.doi 10.1130/G37587.1
dc.description.abstract The current view regarding the timing of regionally developed penetrative tectonic fabrics in sedimentary rocks is that their development postdates lithification of those rocks. In this case, fabric development is achieved by a number of deformation mechanisms, including grain rigid body rotation, crystal-plastic deformation, and pressure solution. The latter is believed to be the primary mechanism responsible for the domainal structure of cleavage in low-grade metamorphic rocks. In this study we combine field observations with strain studies to characterize considerable (>50%) Acadian crustal shortening in a Devonian clastic sedimentary sequence from southwest Ireland. Despite these high levels of shortening there is a marked absence of the domainal cleavage structure and intraclast deformation that are expected with this level of deformation. Fabrics in these rocks are predominantly a product of rigid body rotation and repacking of extraformational clasts during deformation of a clastic sedimentary sequence before lithification was complete. en
dc.format.mimetype application/pdf en
dc.language.iso en en
dc.publisher Geological Society of America en
dc.relation.uri https://pubs.geoscienceworld.org/gsa/geology/article/44/4/291/132050/prelithification-and-synlithification-tectonic
dc.rights © 2016 Geological Society of America. en
dc.subject Clastic rocks en
dc.subject Sedimentary rocks en
dc.subject Europe en
dc.subject Kerry Ireland en
dc.subject Deformation foliation en
dc.subject Devonian en
dc.subject Dingle Peninsula en
dc.subject Ireland en
dc.subject Tectonics en
dc.subject Paleozoic en
dc.subject Western Europe en
dc.title Prelithification and synlithification tectonic foliation development in a clastic sedimentary sequence en
dc.type Article (peer-reviewed) en
dc.internal.authorcontactother Patrick Meere, School Of Biological, Earth & Environmental Sciences, University College Cork, Cork, Ireland. +353-21-490-3000 Email: p.meere@ucc.ie en
dc.internal.availability Full text available en
dc.date.updated 2018-05-31T15:19:00Z
dc.description.version Accepted Version en
dc.internal.rssid 439766071
dc.description.status Peer reviewed en
dc.identifier.journaltitle Geology en
dc.internal.copyrightchecked No !!CORA!! en
dc.internal.licenseacceptance Yes en
dc.internal.IRISemailaddress p.meere@ucc.ie en


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