Revised Manuscript 8/7/12 Click here to view linked References 1 2 3 4 5 The Dalradian rocks of the central Grampian 6 7 Highlands of Scotland 8 9 10 J.E. Treagus, P.W.G. Tanner, P.R. Thomas, R.A. Scott and D. 11 12 Stephenson 13 14 15 Jack E. Treagus 15 Raynham Avenue, Didsbury, Manchester M20 6BW; 16 formerly Department of Earth Sciences, University of Manchester. 17 P.W. Geoff Tanner Department of Geographical and Earth Sciences, 18 University of Glasgow, Gregory Building, Lilybank Gardens, Glasgow 19 G12 8QQ. 20 Peter R. Thomas (deceased) formerly Department of Civil 21 Engineering, Paisley College of Technology. 22 Robert A. Scott Cambridge Arctic Shelf Programme, West Building, 23 181a Huntingdon Road, Cambridge CB3 0DH. 24 25 * David Stephenson British Geological Survey, Murchison House, 26 West Mains Road, Edinburgh EH9 3LA. 27
[email protected] 28 0131 650 0323 29 30 * Corresponding author 31 32 Keywords: 33 Geological Conservation Review 34 Central Grampian Highlands 35 Dalradian Supergroup 36 Lithostratigraphy 37 Structural Geology 38 Metamorphism 39 40 41 42 ABSTRACT 43 44 The Central Grampian Highlands, as defined here, are bounded to the 45 north-west by the Great Glen Fault, to the south-west by Loch Etive 46 and the Pass of Brander Fault and to the south-east by the main 47 outcrop of the Loch Tay Limestone Formation. The more arbitrary 48 northern boundary runs north-west along the A9 road and westwards 49 to Fort William. The detailed stratigraphy of the Dalradian 50 Supergroup ranges from the uppermost Grampian Group through to the 51 top of the Argyll Group, most notably seen in the two classic areas 52 of Loch Leven-Appin and Schiehallion–Loch Tay; Southern Highland 53 Group strata are preserved only in a small structural inlier south 54 of Glen Lyon.