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A Note on Greisening in the Bodmin Moor Granite

By: Exley, C. S.
Material type: ArticleArticleDescription: 427-430pp ; Illustration.Subject(s): Petrology - United Kingdom In: Geological magazine : Vol. 98 Iss. 1-6 Year. 1961Summary: 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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Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002546_55
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002546

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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