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承德大乌苏沟含钒钛磁铁矿矿床地质特征与控矿因素探讨

Gongyong SHENG,Jingwei CHEN,Haitao WANG,Qiuping WANG,Jiaojiao YAO,Binglong ZHOU

Mineral Resources and Geology（2017）

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Abstract
大乌苏沟含钒钛磁铁矿位于河北省承德市大庙一带,地处华北地台北缘燕山台褶带和内蒙地轴的交接地带,大乌苏沟铁矿受红石砬—大庙的深断裂及次级构造和大庙斜长杂岩体控制,成矿构造以NE向压扭性构造为主,NW向压扭性构造次之.矿体成群产出,形状多成脉状、似层状,具有雁行叠瓦式分布产出规律.主要有致密块状矿石组成,矿石结构主要为格状溶离结构、海绵陨铁结构;矿石多为块状和浸染状构造.
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Key words
V-Ti magnetite deposit,geological characteristics,ore-controlling factors,prospecting direction,Dawusugou,Chengde
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