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University of Leeds

The origin of recumbent fold nappes: The Lochalsh fold as the main example

Abstract

dc:description.abstract

This thesis describes structural studies of the Kishorn and Balmacara Nappes of Northwest Scotland and the Mellene Nappe of southern central Norway. These studies have involved the mapping of the orientation, age and distribution of cleavages related to recumbent folding. Using a variety of techniques, including grain shape analysis, measurement of conglomerate pebbles, magnetic anisotropy and palaeomagnetism strain patterns have been obtained for these nappes. Different rock types control the style of folding, and, in part, the sequence of structures developed. The development of. each recumbent fold is a multistage process and prior to each change of mechanism the rate of the current meahanism declines. It is suggested that each change of mechanism is an attempt by the developing structure to maintain the displacement rate required by the thrust belt as a whole. The suggested model for the development of the bedding parallel fabric seen in these nappes indicates the dominance of simple shear deformation on the overturned limbs of recumbent folds. In recumbent fold nappes the passage of the thrust tip into undeformed strata is preceded by folding. The relative ease of lateral propagation may be indicated by the presence or absence of extension parallel to the fold axis or, the presence of layer normal shear strains depending upon the style of folding. The Skarvemellen Anticline or the Mellene Nappe is a non-cylindrical fold with a marked extension lineation parallel to the fold axis. It is thought that this extension lineation results from restriction to the lateral propagation of the fold and thrust. There is an average of 40% extension parallel to the fold axis of the Skarvemellen Anticline in contrast to the Lochalsh Syncline which is a relatively cylindrical fold with relatively little extension parallel to the fold axis, less than 10%.

Degree

thesis:*
Name dc:type.qualificationname
Ph.D
Level dc:type.qualificationlevel
doctoral
Grantor dc:publisher.institution
University of Leeds
Year dc:date.issued
1983

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Potts , Graham John
Advisor dc:contributor.advisor
  • Coward, M.

Identifiers

dc:identifier.*
Identifier
uk.bl.ethos.345263
OAI identifier oai:identifier
oai:etheses.whiterose.ac.uk:1582

Chain of custody

source
Harvested from
White Rose University Consortium
Base URL
etheses.whiterose.ac.uk/cgi/oai2
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
related terms
citation

Potts , Graham John. The origin of recumbent fold nappes: The Lochalsh fold as the main example. doctoral thesis, University of Leeds, 1983.