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Journal of the Geological Society; 1991; v. 148; issue.1; p. 173-180;
DOI: 10.1144/gsjgs.148.1.0173
© 1991 Geological Society of London

Article

A geological and tectonic cross-section of the Caledonides of western Ireland

P. D. RYAN1,2 & J. F. DEWEY1

1 Department of Earth Sciences, The University, Parks Road, Oxford, OX1 3PR, UK
2 Department of Geology, University College, Galway, Ireland

Geological and geophysical criteria allow division of the Caledonides of western Ireland into four principal zones. Zone 1, in the north, contains Grenvillian basement with late Proterozoic supra-crustals. Zone 2 contains the Westport Complex, the Deer Park Complex and the South Mayo Trough. Connemara and the Delany Dome Formation occupy Zone 3. Zone 4 contains the South Connemara Group and mid- to late-Ordovician and Silurian sediments and volcanic rocks. The various tectonic models proposed for these zones are discussed and a ‘minimum’ tectonic model is presented, which involves early Ordovician collision of the northern part of Zone 2 with the Laurentian margin (Zone 1) followed by subduction flip (northern part of Zone 4). The site of early collision between Zones 1 and 2 subsequently underwent orogenic collapse and strike-slip dismemberment leading to the sinistral transpressive emplacement of Zone 3. Assemblages in Zone 4 were accreted to the now south-facing arc. Northwards stress transfer consequent on suturing deformed the thinned crust and overlying Silurian sequences in Zones 2 and 3.




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