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Di laman Kianit:
"Kianit terjadi dalam gneis, syis, pegmatit, dan telerang quarza disebabkan oleh tekanan metamorfisme utama batuan pelit setempat yang tinggi.[perlu rujukan] Ia dijadikan sebagai butiran gersik dalam batuan enap.[perlu rujukan] Ia terjadi disampingkan staurolit, andalusit, silimanit, talkum, hornblend, gedrit, mulit dankorundum.
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