| Reference Type | Journal (article/letter/editorial) |
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| Title | New Rb–Sr and U–Pb ages for the Carnsore Granite and their bearing on the antiquity of the Rosslare Complex, southeastern Ireland |
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| Journal | Geological Magazine |
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| Authors | O'Connor, P. J. | Author |
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| Kennan, P. S. | Author |
| Aftalion, M. | Author |
| Year | 1988 (January) | Volume | 125 |
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| Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800009341Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 253756 | Long-form Identifier | mindat:1:5:253756:0 |
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| GUID | 0 |
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| Full Reference | O'Connor, P. J., Kennan, P. S., Aftalion, M. (1988) New Rb–Sr and U–Pb ages for the Carnsore Granite and their bearing on the antiquity of the Rosslare Complex, southeastern Ireland. Geological Magazine, 125 (1) 25-29 doi:10.1017/s0016756800009341 |
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| Plain Text | O'Connor, P. J., Kennan, P. S., Aftalion, M. (1988) New Rb–Sr and U–Pb ages for the Carnsore Granite and their bearing on the antiquity of the Rosslare Complex, southeastern Ireland. Geological Magazine, 125 (1) 25-29 doi:10.1017/s0016756800009341 |
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| In | (1988, January) Geological Magazine Vol. 125 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractA 12-point whole-rock Rb–Sr isochron for the Carnsore Granite of southeastern Ireland yields an age of 428±11 Ma and initial 87Sr/86Sr ratio of 0.7068±0.0003 (index of goodness of fit, MSWD = 0.65). A similar mean 207Pb/206Pb age of 432±3 Ma from three slightly discordant zircon size fractions from the granite is also indicated, and shows that the pluton was emplaced contemporaneously with the neighbouring Saltee Granite.Thus, Tuskar Group rocks, which are intruded by the Carnsore Granite, could be as young as Ordovician. While the early history of the Rosslare Complex is undoubtedly Precambrian, the new age for the Carnsore pluton means that the later intrusive and tectonothermal events in the history of this complex are no longer constrained to be Precambrian and may have occurred over a 150 + Ma interval in Cambro-Ordovician time.The zircons from the Carnsore Granite are slightly discordant, and show no apparent inherited radiogenic lead component. The initial 87Sr/86Sr ratio suggests that the magma may have been derived as a melt in the lower crust. The higher strontium isotope ratios of the Rosslare gneisses would seem to preclude their involvement in the genesis of the Carnsore magma. |
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