由超高压变质岩组成的变质带，简称为超高压变质带。超高压变质岩是板块俯冲—碰撞作用的产物，是研究板块会聚边界物质组成、结构及地球动力学的重要窗口之一。
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大别山超高压变质带中变质花岗岩常与榴辉岩密切伴生。
As the important member in Dabie ultrahigh pressure metamorphic belt, meta-granitoids are often associated with coesite-bearing eclogites.
大别山高-超高压变质带中的变质花岗岩类是碱性花岗岩。
The metagranitoid found in the high ultrahigh pressure metamorphic belt ( HP UHPMB ) in the Dabie Mountains is alkali meta granite.
在空间分布上，超高压变质带集中于欧亚大陆及其周缘，澳洲和北美目前尚未有报道。
According to present data UHPM rocks are spatially concentrated within Eurasia and at its margins. However, there is still lack of information for North America and Australia.
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