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Intrusion of Cone-Sheets

Published online by Cambridge University Press:  01 May 2009

Ph. H. Kuenen
Ph. H. Kuenen
Affiliation:
Geological Laboratory, Groningen, Holland.
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Summary

Evidence from Mull and Ardnamurchan is brought forward to show that the injection of cone-sheets is accompanied by a vertical lifting of the upper wall. This confirms Anderson's explanation. It is argued that the fracturing and injection are of a quite sudden character and that it is in the nature of the process that no evidence from recent volcanoes has yet been obtained of contemporary cone-sheet injection.

Type
Original Articles
Information
Geological Magazine , Volume 74 , Issue 4 , April 1937 , pp. 177 - 183
Copyright
Copyright © Cambridge University Press 1937

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References

REFERENCES

Harker, A., “The Tertiary Igneous Rocks of Skye,” Mem. Geol. Surv., Scotland, 1904.Google Scholar
Bailey, E. B., etc. “Tertiary and Post-Tertiary Geology of Mull, Loch Aline, and Oban,” Mem. Geol. Surv., Scotland, 1924.Google Scholar
Richey, J. E., “The Geology of Ardnamurchan, North-West Mull and Coll,” Mem. Geol. Surv., Scotland, 1930.Google Scholar
Richey, J. E., “Summary of the Geology of Ardnamurchan,” Proc. Geol. Ass., xliv, 1–56, 1933.CrossRefGoogle Scholar
Richey, J. E., “Guide to the Geological Model of Ardnamurchan,” Mem. Geol. Surv., Scotland, 1934.Google Scholar