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A case of epitaxic replacement

Published online by Cambridge University Press:  14 March 2018

Ivan Kostov
Ivan Kostov*
Affiliation:
Dept. of Mineralogy, University of Sofia
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Summary

Quartz from a granite pegmatite near Kalkovo, Bulgaria, has undergone partial replacement by biotite along cracks parallel to (01;0); the biotite is in regular orientation relative to the quartz, and appears to constitute an instance of epitaxic replacement, defined as a replacement in which the replacing mineral develops in a regular, structurally controlled orientation relative to the mineral replaced.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 31 , Issue 235 , December 1956 , pp. 333 - 338
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1956

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