On the Significance of Thermal Structure in the Scottish Highlands
By: Kennedy, W.Q
.
Material type: 
ArticleDescription: 229 - 234 pp ; Illustration.Subject(s): Thermal structure - Scottish highland - Great Britain | Tectonics - Scottish highland - Great Britain
In:
Geological magazine : Vol. 85 Iss. 1-6 Year. 1948Summary: The formation of a fold mountain chain is, essentially, a thermal phenomenon, as may be deduced from the internal locus of the forces involved, the frequent association of magrriatic activity with erogenic movements, and the widespread thermal and regional metamorphism of the sediments within the deeper parts of the mountain belt.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
|
Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002559_41 | ||
Serials/Scientific Journal
|
Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002559 |
The formation of a fold mountain chain is, essentially, a thermal phenomenon, as may be deduced from the internal locus of the forces involved, the frequent association of magrriatic activity with erogenic movements, and the widespread thermal and regional metamorphism of the sediments within the deeper parts of the mountain belt.
There are no comments for this item.