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A camptonitic dyke suite at monar, ross-shire and inverness-shire

By: Ramsay, John G.
Material type: ArticleArticleDescription: 297-309p ; Illustration.Subject(s): Camptonitic dyke - Loch monar - Western Scotland | Camptonitic dyke - Monar - Ross shire | Camptonitic dyke - Monar - Inverness shire | Petrology | Igneous rock | Rock description - Scotland In: Geological magazine : Vol. 92 Iss. 1-6 Year. 1955Summary: Abstract A swarm of basaltic and camptonitic dykes in the Northern Highlands of Scotland has been studied. The dykes include monchiquite, olivine basalt, olivine dolerite, and camptonite, and a study of the relations of the various types in individual dykes suggests that the camptonites have arisen by the crystallization of late fractions from a magma of fairly normal dolerite type.
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Item type Current location Collection Call number Status Date due Barcode
Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002543_41
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002543

Abstract
A swarm of basaltic and camptonitic dykes in the Northern Highlands of Scotland has been studied. The dykes include monchiquite, olivine basalt, olivine dolerite, and camptonite, and a study of the relations of the various types in individual dykes suggests that the camptonites have arisen by the crystallization of late fractions from a magma of fairly normal dolerite type.

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