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Metaconglomerate rocks are metamorphic rocks that form from the recrystallization of conglomerate rocks under high heat and pressure. They typically have a banded appearance due to the reorientation of minerals like quartz, feldspar, and mica. Metaconglomerates often have a medium to coarse grain size and exhibit strong foliation due to the alignment of mineral grains during metamorphism.

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Q: What are the physical properties of metaconglomerate rocks?
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