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地球学报  2003 

辽西阜新金—多金属成矿区主要断裂带构造特征及其控矿作用

Keywords: 阜新,韧-脆性剪切带,金多金属矿,构造控矿作用

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Abstract:

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。

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