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Note on the Tectonic Style of the Ord Ban Quartzites, Mid-Strathspey

Published online by Cambridge University Press:  01 May 2009

Donald B. McIntyre
Donald B. McIntyre
Affiliation:
(University of Edinburgh)
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Abstract

Study of profiles, perpendicular to the fold-axes, shows that the folding is disharmonic. Nearly every s−surface is one of décollement. In some exposures the quartzites are reduplicated by superposed recumbent-folds without infolds of other material. The contacts are tectonic and not stratigraphic. Incipient boudinage is frequent, and nearly all surfaces show well-developed b−lineation.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 1 , February 1951 , pp. 50 - 54
Copyright
Copyright © Cambridge University Press 1951

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References

REFERENCES

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