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Contact Phenomena from N.W. Jersey, C.I

Published online by Cambridge University Press:  01 May 2009

F. A. Henson
F. A. Henson
Affiliation:
Department of Geology, The University, Nottingham.
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Abstract

The field relationships between the Armorican granite of North-West Jersey and the Precambrian sediments in the Le Pulec and L'Etacq areas are described together with the petrography of the contact rocks. Trace-element determinations on rocks from two traverses across contacts in the area, and upon control specimens of granite and sediments supplement the petrography. The mechanism of granite emplacement in this area is discussed.

Type
Articles
Information
Geological Magazine , Volume 93 , Issue 6 , December 1956 , pp. 473 - 484
Copyright
Copyright © Cambridge University Press 1956

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References

REFERENCES

Groves, A. W., 1930. The Heavy Mineral Suites and Correlation of the Granites of Northern Brittany, the Channel Islands and the Cotentin. Geol. Mag., lxvii, 218–240.CrossRefGoogle Scholar
Henson, F. A., 1947. The Granites of South-West Jersey. Geol. Mag., lxxxiv, 273–280.CrossRefGoogle Scholar
Plymen, G. H., 1921. The Geology of Jersey. Proc. Geol. Assoc., xxxii, 1951, 172.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.; xlii, 178–215.CrossRefGoogle Scholar