The geology of lower Glen Lyon
Glen Lyon forms one of the key areas of Dalradian geology, lying as it does between the inverted stratigraphy of the Tay Nappe 'flat belt', and the Boundary Slide. Historically, work by D. M. Ramsay (1959) interpreted the area as mostly lying on the upper inverted limb of a major recumbent...
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University of Manchester
1984
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.582018 |