The Geology of the Islands of South Connemara
AbstractThe exposed part of the metamorphic envelope on the south side of the Galway granite is described. It is characterized by the presence of pillow lavas and a thick greywacke series containing intraforma-tional conglomerates. This South Connemara Series is tentatively assigned to the Ordovician; such a correlation would require the Galway granite to be a laconic intrusion.
2004 ◽
Vol 13
(2)
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pp. 83-90
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1897 ◽
Vol 4
(4)
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pp. 402-407
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2006 ◽
Vol 36
(6)
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pp. 1085-1103
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