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Contrasted Styles of Folding in the Rocks of Ord Ban Mid-Strathspey1

Published online by Cambridge University Press:  01 May 2009

L. E. Weiss ,
Donald B. McIntyre  and
Martin Kürsten
L. E. Weiss
Affiliation:
Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh 9.
Donald B. McIntyre
Affiliation:
Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh 9.
Martin Kürsten
Affiliation:
Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh 9.
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Abstract

On Ord Ban, quartzite in superposed recumbent folds trending north–south is separated by a slide from mica-schist, granulite, and marble folded in monoclines trending east–west. The reasons for distinguishing between these two styles of folding are given, and the characters of the two styles are contrasted. A fold in quartzite and a fold in marble are described in detail, and kinematic interpretations are attempted. It is concluded that evidence of an early deformation involving mylonitization has been preserved in the quartzite, and that the latest tectonic event distinguishable was the production of the monoclines with attendant twinning of calcite and dolomite.

Type
Articles
Information
Geological Magazine , Volume 92 , Issue 1 , February 1955 , pp. 21 - 36
Copyright
Copyright © Cambridge University Press 1955

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Footnotes

1

Locality map, McIntyre and Turner, 1953, text-fig. 1.

References

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