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Chemical and Mineralogical Changes Associated with the Laxfordian Metamorphism of Dolerite Dykes in the Scourie-Loch Laxford Area, Sutherland, Scotland

  • D. J. Burns (a1)
Abstract

Chemical analyses of dolerites and metadolerites from the Scourie-Loch Laxford area have been made, together with analyses of amphiboles and a pyroxene from these rocks.

Chemical variation within the dykes as originally emplaced has been investigated. Introduction of material during metamorphism is limited, only potassium showing a marked increase in concentration. In the least-altered dykes a relationship between degree of clouding in felspar and amount of H2O+ present is indicated.

Chemical analyses and optical properties of amphiboles show no distinctive trends which could be associated with the progress of the metamorphism.

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References
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MacGregor, A. G., 1931. Clouded felspars and thermal metamorphism. Miner. Mag., 22, 524538.
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O'Hara, M. J., 1961. Petrology of the Scourie Dyke, Sutherland. Miner. Mag., 32, 848865.
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Sutton, J. and Watson, J., 1951. The Pre-Torridonian metamorphic history of the Loch Torridon and Scourie areas in the N.W. Highlands and its bearing on the chronological classification of the Lewisian. Quart. J. geol. Soc. Lond., 106, 241296.
Teall, J. J. H., 1885. The metamorphism of dolerite into hornblende-schist Quart. J. geol. Soc. Lond., 41, 133144.
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Geological Magazine
  • ISSN: 0016-7568
  • EISSN: 1469-5081
  • URL: /core/journals/geological-magazine
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