摘要
河元背地区位于相山矿田西部,由北东向王龙—土塘、小陂—芜头断裂,北西向西山—当前、东堆—社背断裂围限形成河元背菱形断块。近几年,通过对河元背菱形断块内已落实的湖港、河元背和牛头山铀矿床的成矿特征进行总结,对比分析相邻的居隆庵菱形断块内矿床成矿规律并进行钻探查证,在河元背地区新发现了受南北向苦命山—小陂断裂带控制的河元背铀矿床8号带,取得较好的找矿效果。
Heyuanbei area is located in the western part of Xiangshan uranium orefield and is composed of rhombus fault blocks formed by NE-trending Wanglong-Tutang,Xiaopi-Wutou and NW-trending Xishan-Dangqian,Dongdui-Shebei faults. In recent years,through summarizing mineralization characteristics of Hugang Heyuanbei and Niutoushan uranium deposits confirmed in the Heyuanbei rhombus fault block,analyzing and comparing the adjacent metallogenic regularity of the deposits in the Julongan rhombus fault block and drilling checking,the 8 th belt controlled by Kumingshan-Xiaopo fault in Heyuanbei uranium deposits has been implemented to get better prospecting results.
作者
何丹丹
高梦奇
韩园园
HE Dan-dan;GAO Meng-qi;HAN Yuan-yuan(No.270 Research Institute of Nuclear Industry,Nanchang county 33020)
出处
《矿产勘查》
2018年第3期357-366,共10页
Mineral Exploration
基金
中国核工业地质局地勘项目(编号:201631)资助
关键词
苦命山—小陂断裂带
钻探查证
河元背铀矿
相山铀矿田
Kumingshan-Xiaopi fault belt
drilling check
Heyuanbei uranium deposits
Xiangshan uranium orefield
