Age, Geochemistry and Origin of the Ardara Appinite Plutons, Northwest Donegal, Ireland
Abstract
In northwest Donegal, Ireland, a large number of coeval appinitic (hornblende-plagioclase-rich) plutons and lamprophyre dykes occur around the Ardara pluton, a granitic satellite body and one of the oldest phases of the ca. 428–400 Ma composite Donegal Batholith. The appinite units form a bimodal (mafic–felsic) suite in which hornblende is the dominant mafic mineral and typically occurs as large prismatic phenocrysts within a finer grained...
Paper Details
Title
Age, Geochemistry and Origin of the Ardara Appinite Plutons, Northwest Donegal, Ireland
Published Date
Mar 29, 2019
Journal
Pages
31 - 48
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