sheets. This deformation was accompanied by retrogression to amphibolite facies and subsequently locally to greenschist facies.

Torridonian sediments

The Torridonian is a sequence of Neoproterozoic sediments, mainly sandstones that rest unconformably on an old land surface, with up to 300 m of relief locally. The Torridonian is divided into the older Stoer Group and the younger Sleat and Torridon Groups separated by an angular unconformity. Paleomagnetic data

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