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通过对山西义兴寨金矿床成矿构造动力学条件的分析和研究，得出了以下认识：矿床的成矿作用可被划分为脆性破裂和脆韧性张开两个阶段。其中断裂的脆性构造动力学条件在成矿作用早期控制成矿体系内的成矿反应快速进行，沉淀出体系物质；断裂的脆韧性构造动力学条件在成矿作用的中晚期控制成矿反应缓慢进行，分异沉淀出体系物质。在这两种构造动力学环境中形成元素金的两种赋存状态即包体金（晶隙金）和裂隙金
Through the analysis and study of the ore-forming tectonic conditions in the Yixingzhai gold deposit in Shanxi Province, the following conclusions have been reached: The mineralization of the ore deposit can be divided into two stages: brittle fracture and brittle-ductile fracture. The brittle tectonic conditions of the faults controlled the ore-forming reaction in the metallogenic system at the early stage of metallogeny and quickly precipitated out the system materials. The brittle-ductile tectonic kinetic conditions of fracture controlled the mineralization reaction in the middle and late stages of mineralization Slowly, differentiated precipitation system material. In both tectonic dynamics, two kinds of occurrences of elemental gold, inclusions (interstitial gold) and fissured gold