高压变质岩是在俯冲的过程中形成的，从地壳到地幔，深度不等的聚合板块边缘。
High-pressure metamorphic rocks form during subduction of Earth's crust to mantle depths at convergent plate margins.
高压变质岩是在俯冲的过程中形成的，从地壳到地幔，深度不等的聚合板块边缘。
High-pressure metamorphic rocks form during subduction of Earth's crust to mantle depths at convergent plate margins.
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