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Naturally deformed quartz-rich rocks |
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Figure caption |
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undeformed / semibrittle & bulging recrystallization / subgrain rotation recrystallization / grain boundary migration recrystallization |
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25 |
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Less micaceaous Heavitree quartzite; note larger, equant recrystallized grains.The recrystallized grain size is limited by the larger mica grains, although quartz boundaries were able to migrate past smaller mica grains. The distribution of small micas might indicate the characteristic recrystallized grain size at an earlier stage of the deformation-recrystallization. Dislocation creep regime 3. (249 A) |