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A Variety of Quartzite from Craig-choinnich Lodge, near Blair Atholl, Perthshire
Published online by Cambridge University Press: 01 May 2009
Abstract
An unusual variety of quartzite is associated with Dalradian limestone and dark schist at two localities in Upper Glen Fender, near Blair Atholl. The appearance and texture of this quartzite suggest that it is derived from a chert or jasper, and not from a sandstone.
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References
REFERENCES
Bailey, E. B., 1925. Perthshire tectonics: Loch Tummel, Blair Atholl and Glen Shee. Trans. Roy. Soc. Edin., liii, 671–698.CrossRefGoogle Scholar
Barrow, G., Grant Wilson, J. S., and Cunningham Craig, E. H., 1905. The Geology of the country around Blair Atholl, Pitlochry and Aberfeldy. Mem. Geol. Survey.Google Scholar
Peach, B. N., Horne, J., and Teall, J. J. H., 1899. The Silurian Rocks of Britain, Vol. I. Scotland. Mem. Geol. Survey.Google Scholar