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Dyke Phenomena of the Dicq Rock, Jersey, C.I.

Published online by Cambridge University Press:  01 May 2009

M. Casimir  and
Frederick A. Henson
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Abstract

The granite of the Dicq Rock is traversed by several veins of fine grained aplogranite. These in turn are cut by a large dolerite dyke, which has been intruded into a brecciated fault zone within the granite. Three large blocks of granite occur within the dolerite; these originally formed the southern boundary of the fault. The petrography of these rocks, and the influence of the micro-breccia upon the textures found in the marginal and central part of the dolerite, are considered in detail.

Type
Articles
Information
Geological Magazine , Volume 86 , Issue 2 , April 1949 , pp. 117 - 122
Copyright
Copyright © Cambridge University Press 1949

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References

BIBLIOGRAPHY

Noury, C., 1886. Géologie de Jersey. Paris and Jersey.Google Scholar
Wells, A. K., and Wooldridge, S. W., 1931. The Rock Groups of Jersey with Special Reference to Intrusive Phenomena at Ronez. Proc. Geol. Assoc., xlvii, 178–215.CrossRefGoogle Scholar
Mourant, A. E., 1933. The Geology of Eastern Jersey. Quart. Journ. Geol. Soc., lxxxix, 273–307.CrossRefGoogle Scholar
Smith, H. G., 1933. Some Lamprophyres of the Channel Isles. Proc. Geol. Assoc., xliv, 121–130.CrossRefGoogle Scholar
Smith, H. G., 1936. The South Hill Lamprophyre, Jersey. Geol. Mag., lxxiii, 87–91.CrossRefGoogle Scholar
Smith, H. G., 1936. New Lamprophyres and Monchiquites from Jersey. Quart. Journ. Geol. Soc., xcii, 365–383.CrossRefGoogle Scholar
Henson, F. A., 1947. The Granites of South-West Jersey. Geol. Mag. lxxxiv, 273–280.CrossRefGoogle Scholar