Hostname: page-component-78c5997874-lj6df Total loading time: 0 Render date: 2024-11-02T22:51:39.081Z Has data issue: false hasContentIssue false
  • English
  • Français

Conjugate fold systems in the Moine Thrust Zone in the Lochcarron and Coulin Forest areas of Wester Ross

Published online by Cambridge University Press:  01 May 2009

M. R. W. Johnson
M. R. W. Johnson
Affiliation:
Geology Department, Imperial College, London.
Get access Rights & Permissions [Opens in a new window]

Abstract

The Moine Thrust Zone in the Lochcarron and Coulin Forest areas contains numerous small scale folds which plunge eastwards. The axial planes of these folds are inclined towards the north or south so that no regional directional translation of the rocks can be postulated from these structures, whose symmetry as a whole is orthorhombic. The folds are considered to have resulted from local lateral extension and concomitant compression of laminated rocks involved in the thrusting.

Type
Articles
Information
Geological Magazine , Volume 93 , Issue 4 , August 1956 , pp. 345 - 350
Copyright
Copyright © Cambridge University Press 1956

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., 1950. The Structural History of Scotland. Internal. Geol. Congress Report of 18th Session, 1948, part 1, 220–254.Google Scholar
Balk, R., 1952. Fabric of quartzites near thrust faults. Journ. Geol., lx, 415–435.CrossRefGoogle Scholar
Cloos, E., 1946. Lineation. Geol. Soc. Amer. Mem., 18.Google Scholar
Fairbairn, H. W., 1949. Structural Petrology of Deformed Rocks. Cambridge, Mass.Google Scholar
Greenly, E., 1919. The geology of Anglesea. Mem. Geol. Survey Gt. Britain.Google Scholar
Peach, & Horne, , 1907. The Geological Structure of the N.W. Highlands of Scotland. Mem. Geol. Survey, Scotland.Google Scholar
Schmidt, W., 1932. Tectonik und Verformungslehre. Berlin.Google Scholar
Strand, T., 1944. Structural Petrology of the Bygdin Conglomerate. Norsk. Geol. Tidskr., xxiv, 14–31.Google Scholar