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Reversed Graded Beds from the Dalradian of Inishowen, Co. Donegal
Published online by Cambridge University Press: 01 May 2009
Abstract
A sequence of reversed graded beds occurs in a group of flaggy rocks intercalated within the Upper Dalradian grits of Inishowen. Usually these beds have a thickness between ½ inch and 2 inches, and are characterized by a laminated, argillaceous base which grades up into a fine-grained, arenaceous upper member.
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