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A “Luxullianite” from East Dartmoor
Abstract A dyke-like mass of luxullianite type is emplaced along a line of fracture which crosses granite in a zone of pneumatolytic reddening, and is exposed in a quarry face. Extensive tourmalinization is related to post-emplacement fractures which traverse both the luxullianite and the adjacent rocks.
Geological Magazine, Volume 86, Issue 3, June 1949, pp. 175 - 179
Published online by Cambridge University Press: 01 May 2009
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