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New Lamprophyres at Grève de Lecq, Jersey

Published online by Cambridge University Press:  01 May 2009

H. G. Smith
H. G. Smith
Affiliation:
Queen Mary College, London.
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Extract

Grève de lecq is situated on the north coast of Jersey, about 2½ miles from the western end of the island. On each side of the bay is a lamprophyre, discovered by Dr. A. E. Mourant, and the two dykes are so much alike in mineral composition and texture that separate description is unnecessary. The country rock is granite.

Type
Original Articles
Information
Geological Magazine , Volume 76 , Issue 4 , April 1939 , pp. 165 - 170
Copyright
Copyright © Cambridge University Press 1939

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References

LIST OF WORKS TO WHICH REFERENCE IS MADE

(1) Smith, H. G., 1930. “Some Features of Lamprophyres near Sedbergh,” Proc. Geol. Assoc., xli, 336.CrossRefGoogle Scholar
(2) Read, H. H., 1924. “On Certain Xenoliths associated with the Contaminated Rocks of the Huntly Mass, Aberdeenshire,” Geol. Mag., LVI, 1924, 433.CrossRefGoogle Scholar
(3) Bowen, N. L., 1915. “The Later Stages of the Evolution of the Igneous Rocks,” Journ. Geol., Suppl. to xxiii.Google Scholar
(4) Smith, H. G., 1933. “Some Lamprophyrea of the Channel Islands,” Proc. Geol. Assoc., lxiv, 121.CrossRefGoogle Scholar
(5) Smith, H. G., 1936. “New Lamprophyres and Monchiquites from Jersey,” Quart. Journ. Geol. Soc., xcii, 365.CrossRefGoogle Scholar
(6) Sederholm, J. J., 1923. “On Migmatites and associated pre-Cambrian Rocks of S.W. Finland, Part 1,” Bull. Comm. Geol. Finlande, no. 58.Google Scholar
(7) Smith, H. G., 1936. “The South Hill Lamprophyre, Jersey,” Geol. Mag., LXXIII, 87.CrossRefGoogle Scholar
(8) Bowen, N. L., 1922. “The Behaviour of Inclusions in Igneous Magmas,” Journ. Geol., xxx, 513.Google Scholar
(9) Read, H. H. and others, 1926. “Geol. of Strath Oykell and Lower Loch Shin,” Mem. Geol. Surv. Scot.Google Scholar
(10) Flett, J. S., 1929. “The Inverbeg Lamprophyre,” Summ. Prog. Geol. Surv. for 1928, part 2, 29.Google Scholar
(11) Robinson, A. J., and Mourant, A. E., 1936. “Compte rendu de la Réunion Extraordinaire de la Société Géol. et Min. de Bretagne à Jersey,” Mem. Soc. Géol. et Min. de Bretagne, iii, 5.Google Scholar
(12) Read, H. H., 1923. “Geol. of the country round Banff, Huntly, and Turriff,” Mem. Geol. Surv. Scot.Google Scholar
(13) Reynolds, D. L., 1938. “Transfusion Phenomena in Lamprophyre Dykes and their bearing on Petrogenesis,” Geol. Mag., LXXV, 51.CrossRefGoogle Scholar
(14) Read, H. H., 1923. “Petrology of the Arnage District (Aberdeenshire),” Quart. Journ. Geol. Soc., lxxix, 446.CrossRefGoogle Scholar