## Abstract Despite over a century of geological investigation, the Ordovician evolution of South Mayo, western Ireland, is still imperfectly understood. An example of this is the supposed lateral equivalence of two formations within the succession, the Rosroe and Derrylea Formations of Arenig age,
Palaeozoic terrane accretion in the Western Irish Caledonides
β Scribed by Hutton, D. H. W.; Dewey, J. F.
- Book ID
- 119730845
- Publisher
- American Geophysical Union
- Year
- 1986
- Tongue
- English
- Weight
- 676 KB
- Volume
- 5
- Category
- Article
- ISSN
- 0278-7407
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π SIMILAR VOLUMES
The most southerly exposed Lower Palaeozoic strata in Ireland occur on the southwest coast of County Waterford along a 2.5 km long coastal section at Muggort's Bay where they are surrounded by Devonian rocks. Five formations can be distinguished which, in ascending order, are: the Ballycurreen, Carr
Early Palaeozoic bimodal riftβrelated magmatism is widespread throughout much of the Variscides of Europe. It is traceable from the Polish Sudetes to NW Iberia. Granitic plutonism generally predates CambroβOrdovician bimodal magmatism. In the N Bohemian Massif this early Palaeozoic granitic plutonis