A Metamorphic Boundary in the Moine Schists of the Morar and Knoydart Districts of Inverness-shire
By: Lambert, R.St.J
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Material type: 
ArticleDescription: 177 - 194 pp ; Illustration.Subject(s): Metamorphic rock - Moine schists - Morar - Inverness - Shire - Scotland | Metamorphic rock - Moine schists - Knoydart district - Inverness - Shire - Scotland
In:
Geological magazine : Vol. 95 Iss. 1-6 Year. 1958Summary: A re-examination of the Moine—Sub-Moine boundary of the Morar dome shows it to be a zone of transition between two metamorphic states. Some notes on the structure accompany a mineralogical description of the changes across the boundary; discussion is made of evidence that the metamorphic boundary transgresses the geological boundaries. The schists of the core are thought to be in a lower metamorphic state than those of the envelope
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
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Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002550_31 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002550 |
A re-examination of the Moine—Sub-Moine boundary of the Morar dome shows it to be a zone of transition between two metamorphic states. Some notes on the structure accompany a mineralogical description of the changes across the boundary; discussion is made of evidence that the metamorphic boundary transgresses the geological boundaries. The schists of the core are thought to be in a lower metamorphic state than those of the envelope
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