Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-27T20:25:37.106Z Has data issue: false hasContentIssue false
  • English
  • Français

The Ben Lui Recumbent Syncline (S.W. Highlands)

Published online by Cambridge University Press:  01 May 2009

W. A. Cummins  and
R. M. Shackleton
W. A. Cummins
Affiliation:
Department of Geology, University of Liverpool
R. M. Shackleton
Affiliation:
Department of Geology, University of Liverpool
Get access Rights & Permissions [Opens in a new window]

Abstract

Structural evidence from the Ben Lui district supports Bailey's view that the hinge of a major recumbent fold can be demonstrated there. Way up evidence indicates that all the recumbent structures from the Ben Udlaidh fold upwards face towards the south-east and south-south-east. The Ben Udlaidh and Ben Lui folds are therefore synclines. The attitude and character of the folds suggest gravitational flow.

Type
Articles
Information
Geological Magazine , Volume 92 , Issue 5 , October 1955 , pp. 353 - 363
Copyright
Copyright © Cambridge University Press 1955

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.)

References

REFERENCES

Bailey, E. B., and MacGregor, M., 1912. The Glen Orchy Anticline (Argyllshire). Quart. Journ. Geol. Soc., lxviii, 164–179.CrossRefGoogle Scholar
Bailey, E. B., and MacGregor, M., 1922. The structure of the South-West Highlands of Scotland. Quart. Journ. Geol. Soc., lxxviii, 82–127.CrossRefGoogle Scholar
Bailey, E. B., and MacGregor, M., 1938. Eddies in Mountain Structure. Quart. Journ. Geol. Soc., xciv, 607–625.CrossRefGoogle Scholar
Elles, G. L., and Tilley, C. E., 1930. Metamorphism in relation to Structure in the Scottish Highlands. Trans. Roy. Soc. Edin., lvi, pt. iii, 621–646.Google Scholar
Gilmour, P., and McIntyre, D. B., 1954. The Geometry of the Ben Lui Fold (Scottish Highlands). Geol. Mag., xci, 161–6.CrossRefGoogle Scholar
Kennedy, W. Q., 1946. The Great Glen Fault. Quart. Journ. Geol. Soc., cii, 41–76.CrossRefGoogle Scholar
Shrock, R. R., 1948. Sequence in Layered Rocks. New York.Google Scholar
Sitter, L. U. de., 1954. Gravitational Gliding Tectonics. An Essay in Comparative Structural Geology. Amer. Journ. Sci., 252, 321–344.CrossRefGoogle Scholar
Weiss, L. E., McIntyre, D. B., and Kürsten, M., 1955. Contrasted Styles of Folding in the Rocks of Ord Ban Mid-Strathspey. Geol. Mag., xcii, 21–36.CrossRefGoogle Scholar
Wilson, G., 1953. Mullion and Rodding Structures in the Moine Series of Scotland. Proc. Geol. Assoc., lxiv, 118–151.CrossRefGoogle Scholar