【作者】 曾庆栋； 刘建明； 万志民； 于昌明； 叶杰； 刘红涛；

【Author】 ZENG Qingdong~1,LIU Jianming~1 WAN Zhimin~2 YU Changming~1 YE Jie~1 and LIU Hongtao~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Baiyinnuoer Zinc-Lead Deposit,Balin Left Country,Inner Mongolia 025473,China)

【机构】 中国科学院地质与地球物理研究所； 赤峰市白音诺尔铅锌矿；

【摘要】 位于大兴安岭中段的内蒙古赤峰市白音诺尔铅锌矿产于二叠纪黄梁组地层中。矿床矿体主要:呈层状、似层状、透镜状产出控矿因素研究表明,层状、透镜状矿体分布主要受褶皱构造控制。根据褶皱控矿规律指出了三个找矿方向.部分区段得到地球物理验证.白音诺尔铅锌矿床具有良好的成矿前景。更多还原

【Abstract】 The Baiyinnuoer zinc-lead deposit in Chifeng,Inner Mongolia,located at the middle segment of the Da Hinggan Mountains,occurs within the Permian Huanggangliang Group.The orebodies mainly occur as lavered and lenticular shape.Studies on the ore-controlling factors show that distribution of the orebodies is controlled mainly by fold structures.Three exploration ore targets are proposed in accordance with the spatial distribution of the fold structure.The results suggest that the Baiyinnuoer zinc-lead deposit has a potential for further exploration,as validated by geophysical prospecting in the partial area.更多还原