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通过地质构造、显微构造和构造地球化学特征分析 ,论述了辽西阜新金 多金属成矿区主要断裂带的构造特征及其控矿作用 ,并着重指出NEE向、NNE向韧 脆性剪切带是本区主要的控矿和导矿构造 ,而NEE向构造的NW向次级断裂带和NNE向构造的EW向次级断裂带则为本区主要的容矿构造。现已探明的金 多金属矿体也多沿这两个方向展布。
Through the analysis of geological structure, microstructure and tectono-geochemical characteristics, the tectonic characteristics and the ore-controlling functions of the main faults in the Fuxin gold polymetallic metallogenic area in western Liaoning are discussed, and the ductile-brittle shear bands in the NEE direction and NNE are emphasized The main ore-controlling and ore-bearing structures in the area, while the NW sub-fault zone constructed by NEE direction and the EW sub-fault zone constructed by NNE direction are the major ore-hosting structures in this area. The proven gold polymetallic ore bodies are also mostly distributed in both directions.