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The age relationship of the granophyre and basalt of Orval, Isle of Rhum

By: Black, George P.
Material type: ArticleArticleDescription: 106-112p ; Illustration.Subject(s): Age relationship - Granophyre basalt - Orval - Island of Rhum - Scotland | Tertiary plateau lava - Island of Rhum - Scotland | Metamorphism - Basalt - Island of Rhum - Scotland | Petrology - Basalt - Island of Rhum | Historical geology - Scotland In: Geological magazine : Vol. 89 Iss. 1-6 Year. 1952Summary: Abstract On Orval, in the Isle of Rhum, Tertiary plateau lavas directly overlie the granophyre of the ring-complex. Judd considered that the Orval basalts rest unconformably upon an old land surface cut in the granophyre; but on the supposed existence of veining and metamorphism later workers, in particular Geikie and Harker, concluded that the granophyre had intruded the volcanic pile. The author's re-examination of the Orval rocks supports Judd's early interpretation.
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Periodical Section
Bound Journal Collection Not for loan 002540_17
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002540

Abstract
On Orval, in the Isle of Rhum, Tertiary plateau lavas directly overlie the granophyre of the ring-complex. Judd considered that the Orval basalts rest unconformably upon an old land surface cut in the granophyre; but on the supposed existence of veining and metamorphism later workers, in particular Geikie and Harker, concluded that the granophyre had intruded the volcanic pile. The author's re-examination of the Orval rocks supports Judd's early interpretation.

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