The Ballachulish rocks of the Blair Atholl District

Abstract
Synopsis: A succession of quartzites, limestones and pelitic schists formerly correlated with various parts of the Dalradian Supergroup is described in stratigraphic order, determined by sedimentary structures. Lithological similarities indicate correlation with Ballachulish Subgroup rocks and sedimentary structures strongly suggest that the formations described are older than the Blair Atholl Subgroup of the type-locality.

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