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西藏聂拉木高喜马拉雅结晶岩系在区域上以单一的叶理和单一的拉伸线理占主要地位，其变形带的组构主要反映了透入性的伸展变形；根据显微构造分析表明早期由北往南推覆，晚期由南向北伸展，且晚期表现非常明显
The Nyalam high-Himalayan crystalline rock in Tibet is dominated by a single leaf pattern and a single stretching line in the area. The structure of the deformation zone mainly reflects the penetrating extensional deformation. According to the microstructure analysis Early from north to south, the late extension from south to north, and the late performance is very obvious