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一个高压角闪石榴辉岩带出现在豫南─鄂北大别山高压超高压变质单元的最北部。榴辉岩的矿物组合为石榴石＋绿辉石＋角闪石＋绿帘石＋多硅白云母＋石英＋金红石。采用Ｐｏｗｅｌｌ等（１９９４）的Ｔｈｅｒｍｏｃａｌｃ估计的温压条件：压力为１．８－２．４ＧＰａ，温度为４９０－５９２℃。这个带的榴辉岩在矿物组合，矿物成分和温压条件上明显不同于该高压变质单元中其它带的榴辉岩。
A high-pressure hornblende eclogite zone occurs in the northernmost part of the Dabieshan high-pressure and ultrahigh-pressure metamorphic unit in south Henan-northern Hubei. The eclogite mineral assemblage is garnet + omphacite + amphibole + epidote + picein + quartz + rutile. Thermocalc estimated by Powell et al. (1994) was used at a pressure of 1.8-2.4 GPa and a temperature of 490-592 ° C. The eclogites of this zone are significantly different from the eclogites of the other zones in this high-pressure metamorphic unit in terms of mineral assemblage, mineral composition, and temperature and pressure conditions.