内蒙古红花沟金矿床成矿远景评价  

Metallogenic prospect in Honghuagou gold deposit, Inner Mongolia

作　　者：陈伟军[1] 刘红涛[2] 

机构地区：[1]中国科学院研究生院 [2]中国科学院地质与地球物理研究所

出　　处：《黄金》2007年第5期5-9,共5页Gold

基　　金：中国科学院院知识创新工程重要方向项目--大兴安岭典型矿床建模;成矿规律研究及资源远景预测(KZCX-03-SW138)资助

摘　　要：内蒙古红花沟金矿床产于太古代深变质岩中,矿体产出受NW向断裂构造控制,矿石类型主要为石英脉型。EH4连续电导率测量表明,该矿床深部存在明显的地球物理异常,异常强大、清晰,显示了金矿床深部具有良好的成矿前景。Honghuagou gold deposit occurs within Archean metamorphic rocks. Regional or local NW directed faults control the distribution of gold mineralization. The major type of gold mineralization is quartz vein type. The results of EH4 electrical conductivity measurement show that there is a clear geophysical abnormity in the deep part of Honghuagou gold deposit. The abnormity is obvious and visible. It is indicated that Honghuagou gold deposit has a good metallogenic prospect.

关 键 词：石英脉型金矿床 EH4连续电导率测量 红花沟金矿 内蒙古赤峰 

分 类 号：P618.51[天文地球—矿床学]