摘要
内蒙古达茂旗查干诺尔铜矿研究区内构造发育,通过对矿区内构造特征的分析,作者推断矿区范围内较深部位存在整体呈北西向的左行平移断裂、北北东-北北西方向X型共轭剪切断裂,并推断有利铜矿体赋存部位位于Ⅰ号和Ⅳ号矿体之间的中间部位。
The structures developed well in the Chagannuoer copper deposit in Damaoqi, Inner Mongolia. Based on the analysis for the structural characteristics, the author suggest that there are NW direction entire left-lateral wrench faults and NNE -NNW X-type conjugate shear fractures in the deep parts of the deposit, and propose that the ore-forming advantageous position hosts in the middle part between Ⅰ and Ⅳ orebodies.
出处
《地质调查与研究》
2010年第2期130-133,共4页
Geological Survey and Research
基金
内蒙古自冶区地质矿产勘查项目
编号为:200310200030
关键词
构造特征分析
左行平移断裂
X型共轭剪切断裂
查干诺尔铜矿区
内蒙古达茂旗
structural characteristic analyses
left-lateral wrench fault
X-type conjugate shear fracture
Chagannuoer copper deposit
Damaoqi Inner Mongolia
