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Reply to Dewey and Ryan Comment on Searle, MP (2021) ‘Tectonic evolution of the Caledonian orogeny in Scotland: a review based on the timing of magmatism, metamorphism and deformation’

Published online by Cambridge University Press:  05 September 2022

Michael P. Searle Open the ORCID record for Michael P. Searle [Opens in a new window]
Michael P. Searle*
Affiliation:
Department of Earth Sciences, Oxford University, South Parks Road, OxfordOX13 AN, UK Oxford University Museum of Natural History, Parks Road, OxfordOX1 3PW, UK Camborne School of Mines, University of Exeter (Cornwall campus), Penryn, CornwallTR10 9EZ, UK
*
Author for correspondence: Michael P Searle, Email: [email protected]
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Abstract

I welcome the comment from Dewey and Ryan on my paper (Searle, 2021), and the chance to clarify some conflicting Caledonian tectonic models and new ideas. As outlined in the paper, my review was based on the geology of Scotland, not Ireland, Newfoundland or the rest of the Caledonian orogeny beyond, mainly because of length constraints, and the fact that my personal field experience lies mainly in Scotland. The Great Glen fault and the Moine Supergroup are not exposed at all in Ireland, so critical parts, and half of the Caledonian orogeny are missing in Ireland. I argue that the Caledonian geology of Scotland can be explained by a Laurentia – Midland valley arc-microcontinent collision, progressing from NW-directed ophiolite obduction in the Late Cambrian to crustal thickening and regional metamorphism during the Ordovician and Silurian, across the Dalradian and Moine metamorphic rocks. Caledonian structures do continue north into Greenland, as summarized by Leslie et al. (2008), but the geological evolution of the Scottish Caledonides does not require any collision with Baltica. The Dewey and Ryan comment raises major tectonic questions, which this reply addresses.

Keywords

Caledonian orogenyScotlandGreat Glen faultgranitesmetamorphism
Type
Discussion - Reply
Information
Geological Magazine , Volume 159 , Issue 10 , October 2022 , pp. 1837 - 1845
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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