角闪正辉长岩的英文：
hornblende orhtoclase gabbro

Hornblende bearing varieties bridge the gap over to amphibolites which are in bands and dikes
含角闪石的变种填补了带状和脉状角闪岩的中间相。

The micro-gabbro phase is identical with the typical Bulawayan dolerite sills
微辉长岩相与标准的布拉瓦约粒玄岩床相同。

Even foliated metamorphic rocks and banded gabbro can be curved to form folds.
即使变质岩中的片理以及辉长岩中的条带也可产生弯曲而形成褶皱。