张荣,周文博,苏连驰,阳正勇,刘彤,张旭康.内蒙古水泉沟铜多金属矿控矿构造特征研究[J].矿产勘查,2020,11(11):2354-2359 |
内蒙古水泉沟铜多金属矿控矿构造特征研究 |
Study on ore-controlling structural characteristics of Shuiquangou Cu polymetallic deposit, Inner Mongolia |
投稿时间:2020-04-09 |
DOI: |
中文关键词: 铜多金属矿 控矿构造 水泉沟 内蒙古 |
英文关键词: Cu polymetallic deposit, ore-controlling structure, Shuiquangou, Inner Mongolia |
基金项目:中国核工业地质局地质勘查项目(编号:201912)和内蒙古自治区国土资源厅地质勘查专项(编号:05-2-KC95)联合资助。 |
|
摘要点击次数: 1943 |
全文下载次数: 703 |
中文摘要: |
水泉沟矿床褶皱和断裂构造均很发育,近EW向、NE向和近SN向3组断裂构成了区内矿床的基本构造格架。水泉沟铜铅锌银钼多金属矿床共圈出5条矿化带,每条矿化带均受褶皱和断裂构造复合控制。通过矿床地质特征进一步表明,近EW向和NE向断裂交汇部位是矿床的形成有利部位。近EW向断裂、背斜及向斜组合控制着矿体的空间展布,水泉沟多金属矿床受构造控制特征明显。 |
英文摘要: |
The folds and fault structures of the Shuiquangou deposit are well developed. Three groups of faults, near EW, NE and SN, constitute the basic structural framework of the deposit in the area. The Shuiquangou copper-lead-zinc-silver-molybdenum polymetallic deposit has a total of five mineralized zones, and each mineralized zone is controlled by folds and fracture structures. The geological characteristics of the deposit further indicate that the intersection of the near EW and NE faults is a favorable location for the formation of the deposit. The combination of near-EW fault, anticline and syncline controls the spatial distribution of the ore body, and the Shuiquangou polymetallic deposit has obvious structural control characteristics. |
查看全文
查看/发表评论 下载PDF阅读器 |
关闭 |
|
|
|