Hostname: page-component-7dd5485656-frp75 Total loading time: 0 Render date: 2025-10-28T18:30:47.664Z Has data issue: false hasContentIssue false
  • English
  • Français

An Interpretation of Moine-Lewisian Relations in Central Ross-shire

Published online by Cambridge University Press:  01 May 2009

John Sutton  and
Janet Watson
John Sutton
Affiliation:
Department of Geology, Imperial College, London, S.W. 7.
Janet Watson
Affiliation:
Department of Geology, Imperial College, London, S.W. 7.
Get access Rights & Permissions [Opens in a new window]

Abstract

The paper describes those features of the Scardroy Lewisian mass, a sheet-like body of basement rocks thrust into the younger Moine Series, which suggest that this mass was driven up through a thickness of several kilometres of Moinian rocks and inserted as a narrow wedge within the Moine succession, never penetrating the highest members of that succession. The relations of the Scardroy mass, to which most of the Lewisian outcrops of central Ross-shire belong, differ from those of the more westerly outcrops of Lewisian in the region of Glenelg where the basement rocks have been shown by the work of Clough and others to represent wedges lying between tightly-compressed synclines of Moinian rocks which form a more or less autochthonous cover. The connection between the two types of structure is discussed.

Information

Type
Articles
Information
Geological Magazine , Volume 99 , Issue 6 , November 1962 , pp. 527 - 541
Copyright
Copyright © Cambridge University Press 1962

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

REFERENCES

Bailey, E. B., and Tilley, C. E., 1952. Rocks claimed as conglomerates at the Moinian-Lewisian junction. Int. Geol. Congr. Rep. of 18th Session, Gt. Britain, part xiii, 272.Google Scholar
Clifford, P., 1960. The geological structure of the Loch Luichart area, Ross-shire. Quart. J. geol. Soc. Lond., 115, 365–388.CrossRefGoogle Scholar
Clifford, T. N., 1957. The stratigraphy and structure of part of the Kintail district of southern Ross-shire. Quart. J. geol. Soc. Lond., 113, 57–92.CrossRefGoogle Scholar
Clifford, T. N., 1958. A note on kyanite in the Moine Series of southern Ross-shire and a review of related rocks in the Northern Highlands of Scotland. Geol. Mag., 95, 333–346.CrossRefGoogle Scholar
Fallot, P., 1949. Les Chevauchements intercutanés de Roya (A-M). Annales Hébert et Haug (Litre jubilaire Charles Jacob), t. vii, 161–8.Google Scholar
Fallot, P. and Faure-Muret, A., 1949. Sur un mode particulier de charriage. C. R. Ac. Sci. Paris, t. 228, 616–619.Google Scholar
Flett, J. S., 1906. Summ. Progr. geol Surv. G.B. 1905.Google Scholar
Fleuty, M. J., 1961. The three fold systems in the metamorphic rocks of Glen Orrin, Ross-shire. Quart. J. geol. Soc. Lond., 117, 447–79.CrossRefGoogle Scholar
Geikie, A., 1898. Summ. Progr. geol. Surv. G.B. 1897.Google Scholar
Goguel, J., 1952. Traité de Tectonique. Paris.Google Scholar
Kennedy, W. Q., 1955. The tectonics of the Morar anticline and the problem of the north-west Caledonian front. Quart. J. geol. Soc. Lond., 110, 357–390.CrossRefGoogle Scholar
Lambert, R. St.J., 1958. A metamorphic boundary in the Moine Schists of the Morar and Knoydart districts, Inverness-shire. Geol. Mag., 95, 177–194.CrossRefGoogle Scholar
McIntyre, D. B., 1952. The tectonics of the Beinn Dronaig area, Attadale. Trans. Edinb. geol. Soc., 15, 258–264.CrossRefGoogle Scholar
Peach, B. N., and others, 1910. The geology of Glenelg, Lochalsh and the south-east part of Skye. Mem. geol. Surv. U.K.Google Scholar
Peach, B. N. and others, 1913. The Geology of Central Ross-shire. Mem. geol. Surv. U.K.Google Scholar
Peach, B. N. and Horne, J., 1913. The geology of the Fannich Mountains. Mem. geol. Surv. U.K.Google Scholar
Peach, B. N. 1930. Chapters on the Geology of Scotland. Oxford.Google Scholar
Phemister, J., 1960. British Regional Geology. Scotland: the Northern Highlands. 3rd Edit. Geol. Surv. and Mus.Google Scholar
Ramsay, J. G., 1958 a. Superimposed folding at Loch Monar, Ross-shire and Inverness-shire. Quart. J. geol. Soc. Lond., 113, 271–307CrossRefGoogle Scholar
Ramsay, J. G., 1958 b. Moine-Lewisian relations at Glenelg, Inverness-shire. Quart. J. geol. Soc. Lond., 113, 487–520.CrossRefGoogle Scholar
Ramsay, J. G., 1960. The deformation of early linear structures in areas of repeated folding. J. Geol., 68, 75–93.CrossRefGoogle Scholar
Ramsay, J. G., and Spring, J. S., (in press). Moine Stratigraphy in the Western Highlands of Scotland. Proc. Geol. Ass. Lond. 73.Google Scholar
Read, H. H., 1931. The geology of central Sutherland. Mem. geol. Surv. U.K.Google Scholar
Richey, J. E., and Kennedy, W. Q., 1939. The Moine and Sub-Moine Series of Morar, Inverness-shire. Bull. geol. Surv. G.B., 2, 26–45.Google Scholar
Rutledge, H., 1952. The structure of the Fannich Forest Pelitic Belt. Trans. Edinb. geol. Soc., 15, 317–321.CrossRefGoogle Scholar
Sutton, J., 1960 a. Some cross-folds and related structures in northern Scotland. Geol. en Mijnb., 39, 149–163.Google Scholar
Sutton, J., 1960 b. Some structural problems in the Scottish Highlands. Int. Geol. Congr., Report of 21st Session, part xviii, 371–383.Google Scholar
Sutton, J., and Watson, J., 1953. The supposed Lewisian inlier of Scardroy, central Ross-shire and its relations with the surrounding Moine rocks. Quart. J. geol. Soc. Lond., 108, 99–126.CrossRefGoogle Scholar
Sutton, J., 1955. The structure and stratigraphical succession of the Moines of Fannich Forest and Strath Bran. Quart. J. geol. Soc. Lond., 110, 21–54.CrossRefGoogle Scholar
Sutton, J., 1959. Structures in the Caledonides between Loch Duich and Glenelg, North-west Highlands. Quart. J. geol. Soc. Lond., 114, 231–257.CrossRefGoogle Scholar