摘要
内蒙古克什克腾旗查干敖包银铅锌多金属矿为小型中低温热液构造控制矿床,其受近北西向张扭性断裂构造控制,矿体赋存在古元古界锡林郭勒杂岩中。在对该区地质特征分析的基础上,通过与周边邻近的已探明矿床的地质特征进行局部对比,系统分析了该多金属矿的地质特征,讨论了矿床成因及找矿标志,并进一步对该多金属矿区找矿方向和前景进行研究及预测。
The silver-lead-zinc polymetallic deposits in Tsagaan-Obo,Hexigten Banner,Inner Mongolia is a kind of small-size and medium-low temperature hydrothermal structure control deposits.Controlled by near-northwest-direction tensile torsional fault structure,the orebody is stored in SHILINGOL-complex rock body of Paleoproterozoic.Based on the analysis of the geological characteristics of the area and partial comparison with the geological characteristics of the nearby proven deposits,this article systematically analyzes the geological characteristics of the polymetallic deposits,discusses the genesis and prospecting signs of ore deposits,and further investigates and predicts the prospecting direction and prospect of this polymetallic mining area.
作者
王雄飞
郭瑞涛
WANG Xiong-fei;GUO Rui-tao(No.520 team of No.1 Bureau of China General Administration of Metallurgical Geology,Xingtai 054000,China)
出处
《世界有色金属》
2020年第14期77-78,共2页
World Nonferrous Metals
关键词
克什克腾旗
银铅锌多金属矿床
区域背景
矿床成因
找矿方向
Keshiketengqi
Ag Pb Zn polymetallic deposit
regional background
ore genesis
prospecting direction
作者简介
王雄飞,男,生于1987年,汉族,河北邢台人,本科,固体矿产勘查工程师,研究方向:多金属成矿规律及找矿预测。
