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dc.contributor.advisorSevastopulo, George
dc.contributor.authorKeeley, Martin L.
dc.date.accessioned2023-04-20T15:37:58Z
dc.date.available2023-04-20T15:37:58Z
dc.date.issued1980
dc.identifier.citationMartin L. Keeley, 'The carboniferous geology of the Carrick-on-Suir syncline, Southern Ireland', [thesis], Trinity College (Dublin, Ireland). Department of Geology, 1980, pp 354
dc.identifier.otherTHESIS 235
dc.identifier.urihttp://hdl.handle.net/2262/102506
dc.description.abstractA geological map of the Carrick-on-Suir Syncline is presented at a scale of 1:31680 (2 inches to one mile). The thirteen mapping units proposed are discussed in detail; all but the lowermost are Carboniferous in age. The Courceyan transgression of southern Ireland is manifest in the area by a conformable passage from continental elastics (the Kiltorcan Formation), to deep shelf marine micritic accumulations (the Waulsortian Limestone) by way of a suite of transitional facies represented by the Porter's Gate and Hook Head Formations. Though the resulting rock succession is thick (1250m), it has proved susceptible to fine biostratigraphic division using miospores and conodonts.
dc.format1 volume
dc.language.isoen
dc.publisherTrinity College (Dublin, Ireland). Department of Geology
dc.relation.isversionofhttp://stella.catalogue.tcd.ie/iii/encore/record/C__Rb12671803
dc.subjectGeology, Ph.D.
dc.subjectPh.D. Trinity College Dublin 1980
dc.titleThe carboniferous geology of the Carrick-on-Suir syncline, Southern Ireland
dc.typethesis
dc.type.supercollectionthesis_dissertations
dc.type.supercollectionrefereed_publications
dc.type.qualificationlevelDoctoral
dc.type.qualificationnameDoctor of Philosophy (Ph.D.)
dc.rights.ecaccessrightsopenAccess
dc.format.extentpaginationpp 354
dc.description.noteTARA (Trinity's Access to Research Archive) has a robust takedown policy. Please contact us if you have any concerns: rssadmin@tcd.ie


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