New age constraints for the Ordovician Tyrone Volcanic Group, Northern Ireland

New biostratigraphical evidence and a high-precision isotope dilution thermal ionization mass spectrometry U-Pb zircon age provide refined age constraint for the Ordovician Tyrone Volcanic Group of the Tyrone Igneous Complex. In a graptolite fauna from Slieve Gallion, the presence of Isograptus vict...

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Bibliographic Details
Published inJournal of the Geological Society Vol. 165; no. 1; pp. 333 - 339
Main Authors Cooper, Mark R, Crowley, Q. G, Rushton, A. W. A
Format Journal Article
LanguageEnglish
Published London Geological Society of London 01.01.2008
The Geological Society of London
Geological Society
Geological Society Publishing House
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Summary:New biostratigraphical evidence and a high-precision isotope dilution thermal ionization mass spectrometry U-Pb zircon age provide refined age constraint for the Ordovician Tyrone Volcanic Group of the Tyrone Igneous Complex. In a graptolite fauna from Slieve Gallion, the presence of Isograptus victoriae lunatus, the index fossil of the victoriae lunatus graptolite zone, indicates a correlation with the Australasian Castlemainian (Ca1) Stage. The U-Pb zircon age of 473±0.8 Ma dates a volcanic arc-related rhyolite body that is stratigraphically below graptolitic mudstones of Slieve Gallion. The U-Pb isotopic and biostratigraphical age constraints closely match an interpolated age for the base of the Middle Ordovician and indicate a Whitlandian age for the upper Tyrone Volcanic Group, which supports the regional correlation with the Ballantrae Complex, Midland Valley Terrane, Scotland.
ISSN:0016-7649
2041-479X
DOI:10.1144/0016-76492007-057