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On a Dolerite in the Dutch Carboniferous.

Published online by Cambridge University Press:  01 May 2009

S. Tomkeieff
Affiliation:
Armstrong College, Newcastle-on-Tyne
P. Tesch
Affiliation:
Geological Survey, Holland

Extract

In 1928 Dr. P. Tesch published a note on the occurrence of an igneous rock in Dutch Coal-measures (1).1 As this is the first occurrence of an igneous rock in Holland, the present authors have decided to publish a more detailed petrographical description of the rock, together with an attempt to correlate it with similar rocks in Great Britain and Germany.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1931

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References

REFERENCES

(1)Tesch., P.On the occurrence of igneous rocks in the Dutch Carboniferous”: Congrès pour l' Avancement des Études de Stratigraphie Carbonifère. Compte Rendu. Heerlen 7–;11 Juin, 1927. Liege, 1928, 731.Google Scholar
(2)Walker., F.A tholeiitic phase of the quartz-dolerite magma of central Scotland”: Min. Mag., xxii, 1930, 368.Google Scholar
(3)Holmes, A. and Harwood, H. F.. “The tholeiite dikes of the north of England”: Min. Mag., xxii, 1929, 1.Google Scholar
(4)Mockler, G. S.. “A preliminary account of the dykes of Northumberland”: Proc. Univ. Durham Phil. Soc., vii, 1926–7, 244.Google Scholar
(5)Tomkeieff, S. I.. “A contribution to the petrology of the Whin Sill”: Min. Mag., xxii, 1929, 100.Google Scholar
(6)Campbell, R. and Lunn, J. W.. “The tholeiites and dolerites of the Dalmahoy syncline”: Trans. R. Soc. Edinburgh, lv, 1927, 489.CrossRefGoogle Scholar
(7)Holmes, A. and Harwood, H. F.. “The age and composition of the Whin Sill and the related dikes of the north of England”: Min. Mag., xxi, 1928, 493.Google Scholar