It has a prismatic and splintery texture and is abundant in regionally metamorphosed (see metamorphism) rocks such as schists.
具有棱柱形和易碎裂结构,在区域性变质岩(参metamorphism)常丰富,片岩。
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To the schists succeeded gneiss, partially stratified, remarkable for the parallelism and regularity of its lamina, then mica schists, laid in large plates or flakes, revealing their lamellated structure by the sparkle of the white shining mica.
片岩之后是片麻岩,部分分层,因其片层的平行性和规则性而引人注目,然后是云母片岩,铺成大片或片状,通过白闪亮云母的闪光揭示了它们的层状结构。