辽宁省红旗营子铅锌矿床岩脉与含矿构造关系研究  

Research on the relationship between dyke in Hongqiyingzi Pb-Zn deposit in Liaoning province and the mineralized structure

作　　者：董泽龙 张随波 白永俊 王泽 李雪松 

机构地区：[1]辽宁省冶金地质勘查局地质勘查研究院,辽宁鞍山114038

出　　处：《地质找矿论丛》2013年第4期570-575,共6页Contributions to Geology and Mineral Resources Research

摘　　要：文章通过野外对岩脉和含矿构造特征的观察研究,得出它们之间的先后顺序为:NE向花岗斑岩脉→闪长玢岩→矿化构造,NW向岩脉最晚。早期的NE向岩脉为成矿物质提供了运移通道和最佳的容矿空间,并表现为构造矿化带常沿着岩脉产出。Observation and study on geological characteristics of dykes and mineralized structures in Hongqiyingzi Pb Zn deposit show the sequence of NE granite porphyry dyke→diorite porphyrite→mineralized slruclure→NW dyke. The early NE granite porphyry dyke serves as optimum transportation chan- nel of ore fluid and ore hosling space. On the spot of the deposit the structural-mineralized zones generally stretch along the early NE dyke.

关 键 词：红旗营子铅锌矿 含矿构造 岩脉 地质意义 辽宁省 

分 类 号：P588.13[天文地球—岩石学] P613[天文地球—地质学]