The age relationship of the granophyre and basalt of Orval, Isle of Rhum
By: Black, George P.
Material type: ArticleDescription: 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.Item type | Current location | Collection | Call number | Status | Date due | Barcode |
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Article | Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002540_17 | ||
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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