Photomicrograph (crossed polars) of folded schist. The platy, brightly colored minerals are muscovite; the
gray stubbier crystals are quartz. Field of view is approx 1 cm across.
Photomicrograph (crossed polars) of folded schist. The platy, brightly colored minerals are muscovite; the
gray stubbier crystals are quartz. Field of view is approx 1 cm across.
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