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Cone-sheets as a mechanism of uplift

Published online by Cambridge University Press:  01 May 2009

M. J. Le Bas
M. J. Le Bas
Affiliation:
Department of Geology, The University, Leicester, LEI 7RH
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Summary

By the study of dilation associated with cone-sheet emplacement and the deformation of the basal Carboniferous unconformity at the Irish Tertiary igneous centre of Carlingford, it is shown that cone-sheets are capable of producing considerable uplift. This process is also the cause of the steep-sided domes which occur at some carbonatitic centres in Kenya.

Type
Articles
Information
Geological Magazine , Volume 108 , Issue 5 , September 1971 , pp. 373 - 376
Copyright
Copyright © Cambridge University Press 1971

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References

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