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阜平地区位于河北省西部,太行山脉的中段。该处出露的岩层主要是太古宙阜平群。1963年马杏垣教授等在太古宙变质杂岩体构造特征的重要阐述中,曾指出阜平是一个片麻岩穹窿。1965年马杏垣等又对中国东部区域变质作用早于24亿年前后的变质岩系的构造变动类型及形成条件进行了广泛的讨论。其中对阜平穹窿作了专门的阐述。以后,河北、山西两省区调队对该区进行了系统的1:20万区域地质调查,建立了阜平群的层序和构造轮廓。我们在上述工作的基础上对该区构造变形史进行了专题研究。作者选择了阜平县
Fuping is located in the western part of Hebei Province, the middle of the Taihang Mountains. The exposed rock formations here are mainly Archean Fuping Group. In 1963, Professor Ma Xingyuan and other important characteristics of the Archean metamorphic complex description of the complex, had pointed out that Fuping is a gneiss dome. In 1965, Ma Xingyuan et al. Discussed extensively the types of tectonic alterations and the formation conditions of the metamorphic rocks that occurred in China’s eastern region more than 2.4 billion years ago. Fuping Formations which made a special elaboration. Later, the team from Hebei and Shanxi Provinces conducted a systematic 1: 200,000 regional geological survey of the area to establish the sequence and tectonic contour of the Fuping Group. Based on the above work, we conducted a special study on the history of structural deformation in the area. The author chose Fuping County