Abstract
Synopsis Two phases of deformation are responsible for the main structure in an area north of Loch Leven, west of Kinlochleven. The first phase of deformation is associated with the formation of schistosity that is sub-parallel to bedding and relates to large scale overturned folds in the stratigraphy, including the Mamore Syncline. The second phase of deformation corresponds to the development of crenulation cleavage that trends NE-SW to east-west throughout the area. The NE-SW trending bedding and the first schistosity in the north are rotated into north-south in the middle and NNW-SSE in the south of the area by this phase of deformation. The Loch Leven Antiform is, thus, attributed to this stage of deformation. The locally developed third phase deformation may relate to the gentle bending of the second phase fold axes.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.