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Answer :
Final answer:
Schist has a metamorphic texture called foliation, which is characterized by the alignment of mineral grains and gives the rock a banded or layered appearance.
Explanation:
In schist, the metamorphic texture is called foliation. Foliation is the alignment of mineral grains in the rock, which gives it a banded or layered appearance. It is characterized by the parallel arrangement of elongated minerals like micas or amphiboles, or by alternating layers of light and dark minerals.
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