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Metamorphic Differentiation of Talc-Magnesite-Chlorite Rocks in Shetland
Published online by Cambridge University Press: 01 May 2009
Abstract
Practically monomineralic masses of talc, of magnesite, and of chlorite are formed in talc-magnesite-chlorite-rocks as a result of localized shearing and associated hydrothermal activity within deformation-belts.
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