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Zoning in garnets from the mainland Lewisian
Published online by Cambridge University Press: 05 July 2018
Abstract
Two types of zoning are found in garnets from Lewisian rocks. One is due to retrogression of an earlier homogeneous garnet while the other results from growth (or equilibration) during falling temperatures. Both zoning patterns result from metamorphism during or after the Dionard tectonic phase of the Laxfordian event.
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- Copyright © The Mineralogical Society of Great Britain and Ireland 1981
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