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Reverse zoning between myrmekite and albite in a quartzofeldspathic gneiss from Broken Hill, New South Wales
Published online by Cambridge University Press: 05 July 2018
Summary
Grain boundary migration and the exsolution of albite from alkali feldspar, followed by the precipitation of myrmekite from the same source on to adjacent plagioclase grains, will explain the reversed zoning of these phases in contrast to the normal zoning seen in igneous rocks.
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- Research Article
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- Copyright © The Mineralogical Society of Great Britain and Ireland 1974
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