Hostname: page-component-84b7d79bbc-g5fl4 Total loading time: 0 Render date: 2024-07-30T09:09:03.601Z Has data issue: false hasContentIssue false
  • English
  • Français

On the Significance of Thermal Structure in the Scottish Highlands

Published online by Cambridge University Press:  01 May 2009

W. Q. Kennedy
Get access Rights & Permissions [Opens in a new window]

Extract

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.

Type
Articles
Information
Geological Magazine , Volume 85 , Issue 4 , August 1948 , pp. 229 - 234
Copyright
Copyright © Cambridge University Press 1948

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

LITERATURE

Bailey, E. B., 1923. The Metamorphism of the South-Western Highlands of Scotland. Geol. Mag., lx, 317.CrossRefGoogle Scholar
Barrow, G., 1893. On an Intrusion of Muscovite Biotite Gneiss in the S.E. Highlands of Scotland and its Accompanying Metamorphism. Quart. Journ. Geol. Soc., xlix, 330.CrossRefGoogle Scholar
Barrow, G. 1912. The Geology of Lower Deeside and the S. Highland Border. Proc. Geol. Ass., xxiii, 274.CrossRefGoogle Scholar
Elles, G. L., and Tilley, C. E., 1930. Metamorphism of the South-Western Highlands of Scotland. Trans. Roy. Soc. Edinburgh, Ivi, 621.Google Scholar
Goldschmidt, V. M., 1912. Die Kaledonische Deformation der Sud-norwegischen Urgebirgstafel. Vid. Selsk. Skrifter, 1 Mat-Naturv. Klasse, No. 19.Google Scholar
Goldschmidt, V. M. 1915. Die Kalksilikatgneisse and Kalksilikatglimmerschiefer des Trondhjem-Gebiets. Vid. Selsk. Skrifter, 1 Mat-naturv. Klasse, No. 10.Google Scholar
Hess, H. H., 1938. Gravity Anomalies and Island Arc Structure with particular reference to the West Indies. Proc. Amer. Phil. Soc., 79, 71.Google Scholar
Kennedy, W. Q., 1946. The Great Glen Fault. Quart. Journ. Geol. Soc., cii, 41.CrossRefGoogle Scholar
Kuenen, Ph. H., 1937. The Negative Isostatic Anomalies in the East Indies. Leidsche Geol. Med., 8, 169.Google Scholar
Tilley, C. E., 1925. Metamorphic Zones in the Southern Highlands of Scotland. Quart. Journ. Geol. Soc., lxxxi, 100.CrossRefGoogle Scholar
Umbgrove, J. H. F., 1947. The Pulse of the Earth, 2nd Edit.CrossRefGoogle Scholar
Vening, Meinesz F. A., 1934. Gravity Expeditions at Sea, vol. ii. The interpretation of the results (with J. H. F. Umbgrove and Ph. H. Kuenen).Google Scholar