The tectonic gneiss,developed at deep crustal-tectonic levels by grain flow and diffusion creep mechanism,have stripe and band fabrics in macroscopic,and three edges equilibrium texture in microscopic scales.
构造片麻岩系列形成于地壳深部构造层次上,以颗粒流动和扩散蠕变变形机制为主,宏观上表现为条纹和条带状构造,微观上为三边平衡结构。
参考来源 - 变质构造岩类型及其特征·2,447,543篇论文数据，部分数据来源于NoteExpress
构造片岩类，分为构造片岩和构造片麻岩。
Tectonic schist type including tectonic schist and tectonic gneiss.
片麻岩带南北两侧的岩石，在岩性上及构造上都和它大不相同。
Rocks to the north and south of the gneiss zone are lithologically and structurally distinct from it.
在东喜马拉雅构造结南迦巴瓦岩群中，石榴辉石岩呈透镜状产于麻粒岩相变质的长英质片麻岩和泥质片岩之中。
Garnet pyroxenite occurs as lenses in granulite-facies metamorphic granitic gneiss and pelitic schist in the Namjagbarwa Group-complex of the eastern Himalayan tectonic syntaxis.
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