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I.—On Olivine Nodules in the Basalt of Calton Hill, Derbyshire

Published online by Cambridge University Press:  01 May 2009

H. H. Arnold-Bemrose
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Extract

The object of this paper is to place on record the occurrence of olivine nodules in a British basalt which, though closely allied in structure to some of the Tertiary basalts of the Continent, belongs undoubtedly to the Carboniferous age. Olivine nodules frequently occur in the Continental basalts and have been considered by some writers as inclusions of peridotites, but by others as segregations from the magma.

Type
Original Articles
Information
Geological Magazine , Volume 7 , Issue 1 , January 1910 , pp. 1 - 4
Copyright
Copyright © Cambridge University Press 1910

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References

1 “On the Microscopic Structure and Composition of British Carboniferous Dolerites”: Q.J.G.S., 1874, vol. xxx, p. 552.Google Scholar

2 British Petrography, 1888, p. 246.

3 Q.J.G.S., 1894, vol. 1, p. 621.Google Scholar

4 Q.J.G.S., 1907, vol. lxiii, p. 252.Google Scholar