The occurrence of zoisite + kyanite + coesite assemblage indicates that the upper pressure limit of eclogite in the Dabie Mountains does not reach the stability field of lawsonite and therefore could not exceed 4 . 0-4 . 5 GPa .

黝 帘 石 -蓝晶石-柯石英组合的出现指示大别山榴辉岩的压力上限未达到硬柱石的稳定区域，其形成压力不会超过4.0～4.5GPa。

Garnet + phengite + albite + quartz + epidote / zoisite ± barroisite in the muscovite albite ( monzo ) schist and gneiss ;

在白云母钠长（二长）片岩和片麻岩中为石榴石＋多硅白云母＋钠长石＋石英＋绿帘石／ 黝 帘 石±冻蓝闪石；

The mineral assemblages in the main stage are garnet + phengite + quartz + magnetite ± paragonite ± epidote / zoisite in the mica schist ;

主期阶段的矿物组合在云母片岩中为石榴石＋多硅白云母＋石英＋磁铁矿±钠云母±绿帘石／ 黝 帘 石；

This high-pressure metamorphic belt is characterized by the assemblages of high-pressure metamorphic minerals comparing with other veins it composed garnet omphacite phengite zoisite and so on .

该高压变质带以 发育 大量的高压脉为特征。高压脉与其他脉体相比，具有特征的高压变质矿物组合，包括石榴子石、绿辉石、多硅白云母、 黝 帘 石等。