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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Published in | Journal of the Geological Society Vol. 165; no. 1; pp. 333 - 339 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
London
Geological Society of London
01.01.2008
The Geological Society of London Geological Society Geological Society Publishing House |
Subjects | |
Online Access | Get full text |
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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. |
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ISSN: | 0016-7649 2041-479X |
DOI: | 10.1144/0016-76492007-057 |