大连地区褶皱构造式样及叠加变形现象极其丰富。本文从构造解析入手 ,运用微观构造与宏观构造相结合方法 ,详细划分了该区中生代的韧性变形构造期次 ,并研究和确定了各期的变形机制及变形式样 ,提出印支晚期南北向挤压变形为该区中生代发生的第一期韧性变形构造事件。在对全区资料综合分析基础上 ,重新厘定了研究区的构造格局。 Dalian area fold structure patterns and superposition deformation is extremely rich. Beginning with the structural analysis, this paper uses the combination of microstructure and macrostructure to divide the Mesozoic ductile deformation structure in detail and study and confirm the deformation mechanism and deformation pattern of each period. The pressure deformation is the first-stage ductile deformation tectonic event occurred in Mesozoic in this area. Based on the comprehensive analysis of the data of the whole area, the tectonic structure of the study area was redetermined.