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Variation of metamorphic grade in Lower Strathspey
Published online by Cambridge University Press: 01 May 2009
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.
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