The highland border controversy : a discussion of new evidence that the lower cambrian leny limestone at callander, perthshire, belongs to the dalradian supergroup, and a reassessment of the exotic status of the highland border complex
By: Bluck, B.J
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Contributor(s): Ingham, J.K | Tanner, P.W.G.
Material type: 
ArticleDescription: 563-570pp ; Illustration.Subject(s): Stratigraphical correlation | Stratigraphy | Lower palaeozoic | Stratigraphy - Scotland
In:
Geological magazine : Vol. 134 Iss. 1-6 Year. 1997Summary: B. J. Bluck & J. K. Ingham comment: The status of the fossiliferous rocks at the Highland Border (the Highland Border Complex) has been a matter of speculation for over a century. The question has been whether the Highland Border Complex has affinities with the Dalradian block or constitutes a separate block, a sliver or slivers of which have been caught up along the Highland Boundary Fault.
| 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 | 002523_128 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002523 |
B. J. Bluck & J. K. Ingham comment: The status of the fossiliferous rocks at the Highland Border (the Highland Border Complex) has been a matter of speculation for over a century. The question has been whether the Highland Border Complex has affinities with the Dalradian block or constitutes a separate block, a sliver or slivers of which have been caught up along the Highland Boundary Fault.
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