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Deformation and metamorphic reactions in polyphase rocks |
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Figure caption |
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Plagioclase grain from granodiorite moderately deformed at low to mid greenschist conditions, and mostly reacted to a mixture of albite and clinozoisite.More strongly deformed granodiorite, showing a plagioclase grain which has been largely decomposed by neo-mineralization. Mixtures of very fine-grained high-relief clinozoisite and albite are beginning to form interconnected layers, leading to a foliation in the rock. In the upper part of the image, quartz is dynamically recrystallized with a grain size larger than that in the phase mixture. |