Quarzit (z. B.
<Rosa Quarzit>,
<Azul do Macaubas>
) ist ein porenarmes, quarzreiches Ablagerungsgestein (z. B. <Sandsteine>, Quarzkonglomerate) mit kieseligem Bindemittel, das durch Druck und/oder hohe Temperatur zu Quarzit umgewandelt wurde.
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