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Variation of metamorphic grade in Lower Strathspey

Published online by Cambridge University Press:  01 May 2009

J. A. Winchester
J. A. Winchester
Affiliation:
Department of Geology, University of Keele, Keele, Staffs ST5 5BG, U.K.
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Summary

The mineral assemblages in calc-silicates collected from Ballindalloch and Bridge of Avon suggest that the grade of metamorphism is lower than in the areas to the E and W. Mild post-metamorphic warping may be responsible for the production of an apparent ‘thermal anticline’ in the Monadhliath Mountains and the complementary ‘thermal syncline’ in Lower Strathspey.

Type
Articles
Information
Geological Magazine , Volume 117 , Issue 2 , March 1980 , pp. 187 - 189
Copyright
Copyright © Cambridge University Press 1980

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References

Chinner, G. A. 1978. Metamorphic zones and fault displacement in the Scottish Highlands. Geol. Mag. 115, 37–45.Google Scholar
Hinxman, L. W. & Grant Wilson, J. S. 1902. The geology of Lower Strathspey. Mem. geol. Surv. U.K. Sheet 85.Google Scholar
Hinxman, L. W. & Anderson, E. M. 1915. The geology of Mid-Strathspey and Strathdearn. Mem. geol. Surv. U.K. Sheet 84.Google Scholar
Kennedy, W. Q. 1949. Zones of progressive metamorphism in the schists of the Western Highlands of Scotland. Geol. Mag. 86, 43–56.Google Scholar
Lambert, R. StJ. & McKerrow, W. S. 1976. The Grampian Orogeny. Scott. J. Geol. 12, 271–92.Google Scholar
Lambert, R. StJ., Winchester, J. A. & Holland, J. G. 1979. Time, space and intensity relationships for the Precambrian and Lower Palaeozoic metamorphisms of the Scottish Highlands. In The Caledonides of the British Isles – reviewed.Google Scholar
Piasecki, M. A. J. & van Breemen, O. 1979(a). The ‘Central Highland Granulites’: cover-basement tectonics in the Moine. In The Caledonides of the British Isles – reviewed.Google Scholar
Piasecki, M. A. J. & van Breemen, O. 1979(b). A Morarian age for the ‘younger Moines’ of central and western Scotland. Nature, Lond. 278, 734–36.CrossRefGoogle Scholar
Winchester, J. A. 1973. Pattern of regional metamorphism suggests a sinistral displacement of 160 km along the Great Glen Fault. Nature Phys. Sci. 246, 81–4.Google Scholar
Winchester, J. A. 1974(a). The zonal pattern of regional metamorphism in the Scottish Caledonides. Jl geol. Soc. Lond. 130, 509–24.Google Scholar
Winchester, J. A. 1974(b). The three-dimensional pattern of polyphase metamorphism in the Moinian Assemblage of northern Ross-shire. J. Geol. 82, 637–49.Google Scholar
Winchester, J. A. 1978. The zonal pattern of metamorphism in the Scottish Highlands and the displacement along the Great Glen Fault: discussion of paper by Chinner, G. A. Geol. Mag. 115, 453–60.Google Scholar
Winchester, J. A. & Whittles, K. H. 1979. The pattern of three-dimensional metamorphism in the Killin area, Inverness-shire: a direct method of determining the thickness of metamorphic zones in the Caledonides in The Caledonides of the British Isles – reviewed.Google Scholar