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Isotopic age dating records that the latest major pre-Caledonian event in the Annagh Gneiss is of Grenvillian age. All analysed basic rocks fall into three categories: early basic and ultrabasic pods and metadolerite dykes.
The Annagh Division gneiss differs chemically from Laxford gneiss but is similar to reworked Lewisian inliers seen in the N. All originated as minor intrusives of tholeiitic affinities.
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