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Flarengites are a type of rare, high-temperature metamorphic rock that typically forms from the alteration of sedimentary or igneous rocks under extreme conditions. They are characterized by their unique mineral composition, which often includes garnet, kyanite, and other high-pressure minerals. Flarengites are primarily studied in geological contexts to understand the conditions of their formation and the tectonic processes involved. Due to their rarity, they provide valuable insights into the Earth's crust and its evolutionary history.
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