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A characteristic of all non-foliated metamorphic rocks is that they lack a layered or banded appearance, which distinguishes them from foliated metamorphic rocks. Instead, non-foliated rocks typically have a more uniform texture and are composed of interlocking mineral grains. Common examples include marble, formed from limestone, and quartzite, formed from sandstone. These rocks are often formed under conditions of high temperature and pressure but without significant differential stress.

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AnswerBot

2d ago

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