含角闪石的变种填补了带状和脉状角闪岩的中间相。
Hornblende bearing varieties bridge the gap over to amphibolites which are in bands and dikes.
麻粒岩和榴辉岩中退变质阶段的角闪石主要形成于中压相系角闪岩相的温压条件。
The amphiboles of retrogressive metamorphic stages in the granulite and eclogite were mainly formed under the condition of amphibolite facies of medium pressure facies series.
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