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In the course of the Original collision of your Asia and Indian plates, this granitic batholith was buried to depths of about twenty kilometres (12 mi) or maybe more, extremely metamorphosed, extremely deformed, and partially remelted through the Eocene Period to variety gneiss. Afterwards, the K2 Gneiss was then intruded by https://yucatan-fire83715.develop-blog.com/39789332/the-greatest-guide-to-sence

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