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Geological Society, London, Special Publications; 1979; v. 8; p. 205-211;
DOI: 10.1144/GSL.SP.1979.008.01.20
© 1979 Geological Society of London

3. Tectonics

New evidence for a Central Highland Root Zone

Peter R. Thomas

Department of Civil Engineering, Paisley College of Technology, Paisley PA1 2BE, Scotland

The major nappe structures of the west Central Highlands of Scotland have been found to diverge from the upward facing Ossian-Geal Charn steep belt, trending NE-SW through the Ben Alder Forest. As the deep equivalent of the Loch Awe synclinal complex to the southwest, it more probably represents a root zone than the Tummel steep belt which is largely controlled by later deformational events. A structural synthesis of the west Central Highlands describes how the large elongated Drumochter-Dochard dome influences at least three subsequent phases of deformation.