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A Note on Greisening in the Bodmin Moor Granite
Published online by Cambridge University Press: 01 May 2009
Abstract
Some differential weathering of tors on Bodmin Moor has been found to be due to narrow zones of greisen. These zones are not related to the joint system in the granite and appear to have arisen by the alteration of feldspars in the path of escaping late-magmatic fluids.
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