Anatexis is pervasive in high grade metamorphic rocks and has received much attention from geoscientists. 摘要深熔作用在高级变质岩中非常普遍并受到广泛关注。
Subsequent redistribution of uranium in provinces formed at that time most probably resulted from orogenic processes and associated anatexis. 铀在成矿区内的重新分布，最可能是由于造山作用及伴随的泾熔作用。
