ALSOP, G. I. and HOLDSWORTH, R. E. (2002): The geometry and kinematics of flow perturbation folds, Tectonophysics, 350, pp. S.3) is the only structure that disrupts the sequence significantly, although a common succession is recognized in its foot-wall and hanging-wall.

Further north, there seems little doubt that the psammite-dominated succession of western Sutherland equates with the Morar Group ((Fig. From: Strachan, Rob, Friend, Clark, Alsop, Ian, Miller, Suzanne (Editors). Grampian orogenic event – mid to upper amphibolite facies metamorphism and deformation of the eastern Moines above Sgurr Beag and Naver thrusts. (1963): Rb-Sr isotopic ages from the Moine series, in. RAMSAY, J. G. (1962): The geometry and mechanics of ‘similar type folds, Journal of Geology, 70, pp. SMITH, D. I. VAN BREEMEN, O., AFTALION, M., PANKHURST, R. J. and RICHARDSON, S. W. (1979b): Age of the Glen Dessary syenite, Inverness-shire: diachronous Palaeozoic metamorphism across the Great Glen, Scottish Journal of Geology, 15, pp. 43-53. Baltica is thought to have collided with the segment of the Laurentian margin that incorporated the Northern Highlands, to result in the Scandian orogenic event (Fig. BUTLER, R. W. H. (2004b): The nature of ‘roof thrusts’ in the Moine Thrust Belt, NW Scotland: implications for the structural evolution of thrust belts, Journal of the Geological Society, London, 161, pp.

887-903.

Neoproterozoic plate reconstructions mostly depict the continents in close proximity (Fig. READ, H. H. (1961): Aspects of the Caledonian magmatism in Britain, Liverpool and Manchester Geological Journal, 2, pp. Within the Morar Group, many inliers occupy the cores of major sheath folds; thin allochthonous slices of highly strained basement lie along the Ben Hope, Naver and Swordly thrusts (Holdsworth, 1989a). The aim of this excursion guide is to allow geological field parties to see the wide variety of rocks and structures that occur within the outcrop of the Moine Supergroup, as well as the Moine Thrust Zone that separates these rocks from those of the Caledonian foreland to the NW. 807-15. Sm-Nd and U-Pb mineral ages of c.1100-1000 Ma obtained from the eclogite-bearing eastern Glenelg inlier (Excursion 7; Sanders et al., 1984; Brewer et al., 2003) imply that at least some of the basement inliers were reworked during the Grenville orogeny. HUTTON, D. H. W. and MCERLEAN, M. (1991): Silurian and Early Devonian sinistral deformation of the Ratagain granite, Scotland: constraints on the age of Caledonian movements on the Great Glen fault system, Journal of the Geological Society, London, 148, pp. FETTES, D. J. and MACDONALD, R. (1978): The Glen Garry vein complex, Scottish Journal of Geology, 14, pp. S.1) is a more plausible correlative of the Sgurr Beag Thrust (Kocks et al., 2006). A. COWARD, M. P. (1990): The Precambrian, Caledonian and Variscan framework to NW Europe, in HARDMAN, R. F. P. and BROOKS, J.

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