nerc.ac.uk

Stratigraphic, geochemical and U-Pb zircon constraints from Slieve Gallion, Northern Ireland: a correlation of the Irish Caledonian arcs

Hollis, S.P.; Cooper, M.R.; Roberts, S.; Earls, G.; Herrington, R.; Condon, D.J.. 2013 Stratigraphic, geochemical and U-Pb zircon constraints from Slieve Gallion, Northern Ireland: a correlation of the Irish Caledonian arcs. Journal of the Geological Society, 170 (5). 737-752. 10.1144/jgs2012-104

Before downloading, please read NORA policies.
[img]
Preview
Text
Hollis_et_al_2013_Gallion.pdf - Accepted Version

Download (25MB) | Preview

Abstract/Summary

Recent Ar–Ar and U–Pb zircon geochronology from across the British and Irish Caledonides has revealed a prolonged period of arc-ophiolite formation (c. 514–464 Ma) and accretion (c. 490–470 Ma) to the Laurentian margin during the Grampian orogeny. The Slieve Gallion Inlier of Northern Ireland, an isolated occurrence of the Tyrone Volcanic Group, records the development of a peri-Laurentian island arc–backarc and its obduction to an outboard microcontinental block. Although a previous biostratigraphic age constraint provides a firm correlation of at least part of the volcanic succession to the Ca1 Stage of the Arenig (c. 475–474 Ma), there is uncertainty on its exact statigraphic position in the Tyrone Volcanic Group. Earliest magmatism is characterized by light rare earth element (LREE) depleted island-arc tholeiite. Overlying deposits are dominated by large ion lithophile and LREE-enriched, hornblende-phyric and feldspathic calc-alkaline basaltic andesites and andesitic tuffs with strongly negative ϵNdt values. Previously published biostratigraphic age constraints, combined with recent U–Pb zircon geochronology and new petrochemical correlations, suggest that the Slieve Gallion Inlier is equivalent to the lower Tyrone Volcanic Group. Temporal and geochemical correlations between the Slieve Gallion Inlier and Charlestown Group of Ireland suggest that they may be part of the same arc system, which was accreted at a late stage (c. 470 Ma) in the Grampian orogeny. A switch from tholeiitic volcanism to calc-alkaline dominated activity within the Lough Nafooey Group of western Ireland occurred prior to c. 490 Ma, some 15–20 Myr earlier than at Tyrone and Charlestown.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1144/jgs2012-104
ISSN: 0016-7649
Date made live: 20 Nov 2013 14:52 +0 (UTC)
URI: http://nora.nerc.ac.uk/id/eprint/503952

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...