张宣地区的高级片麻岩地体褶皱样式从等斜的片内褶皱、与韧性剪切带紧密伴生的构造，到脆性剪切、开阔褶皱和平缓的弯曲，经历了韧性－脆性的变形．根据构造叠加原理、利用构造间的相互关系可以确定其变形序列，并对断裂构造及其控矿作用进行了探讨 The high-grade gneiss body fold pattern in Zhangxuan area has experienced ductile-brittle deformation from isopachic folds, structures closely associated with ductile shear zones, to brittle shear, open folds and gentle curves. According to the principle of superposition of structures, the sequence of deformation can be determined by the correlation among the structures and the fracture structure and its ore-controlling effect are also discussed