We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Garson, M. S. & Plant, J.1972. Possible dextral movements on the Great Glen and Minch Faults in Scotland. Nature, Lond.240, 31–5.Google Scholar
Kennedy, W. Q.1946. The Great Glen Fault. Q. Jl geol. Soc. Lond.102, 41–72.CrossRefGoogle Scholar
Miller, J. A. & Flinn, D.1966. A survey of age relations of Shetland rocks. Geol. Jl5, 95–116.CrossRefGoogle Scholar
Mykura, W.1972(a). The Old Red Sandstone sediments of Fair Isle, Shetland Island. Bull. geol. Surv. Gt Br.41, 1–31.Google Scholar
Mykura, W.1972(b). Igneous intrusions and mineralization in Fair Isle, Shetland Islands. Bull. geol. Surv. Gt Br.41, 33–53.Google Scholar
Mykura, W. & Phemister, , (In the press.) The geology of western Shetland. Mem. geol. Surv. Gt Br.Google Scholar
Mykura, W., with contributions by Flinn, D. and May, F.M. (In the press.) British Regional Geology: Orkney and Shetland. I.G.S. Regional Guide.Google Scholar
Munro, M.1973. Structures in the south-eastern portion of the Strontian granitic complex, Argyllshire. Scott. Jl Geol.9, 99–108.CrossRefGoogle Scholar
Storetvedt, K. M.1974. A possible large-scale sinistral displacement along the Great Glen Fault in Scotland. Geol. Mag.111, 23–30.CrossRefGoogle Scholar
Winchester, J. A.1973. Pattern of regional metamorphism suggests a sinistral displacement of 160 km along the Great Glen Fault. Nature: Phys. Sci.246, 81–3.Google Scholar