内蒙古复兴屯超大型银铅锌矿床地质特征及找矿标志
Received:December 05, 2021  Revised:July 29, 2023  点此下载全文
引用本文:LI HaiJun,ZHANG ShanMing,LIANG XinQiang,HU ErHong,HAO ZhiHui,WANG YaNan,WU Bin,KANG JianFei,BAI Tao,ZHOU LiJun.2023.Geological characteristics and prospecting indicators of Fuxingtun giant Ag-Pb-Zn deposit in Inner Mongolia[J].Mineral Deposits,42(6):1175~1194
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Author NameAffiliationE-mail
LI HaiJun Inner Mongolia Geological Exploration Institute of Sinochem Geology and Mining Bureau, Hohhot 010000, Inner Mongolia, China  
ZHANG ShanMing School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
Inner Mongolia Mining Development Co. Ltd., Hohhot 010011, Inner Mongolia, China 
shanming.zhang@163.com 
LIANG XinQiang Inner Mongolia Land Resources Exploration and Development Co. Ltd., Hohhot 010020, Inner Mongolia, China  
HU ErHong Inner Mongolia No.8 Geological and Mineral Exploration and Development Co. Ltd., Wuhai 016000, Inner Mongolia, China  
HAO ZhiHui Ordos Geological Survey and Monitoring Institute, Ordos 017000, Inner Mongolia, China  
WANG YaNan Inner Mongolia Geology and Mineral Resources(Group) Co., Ltd., Hohhot 010011, Inner Mongolia, China  
WU Bin Inner Mongolia Geology and Mineral Resources(Group) Co., Ltd., Hohhot 010011, Inner Mongolia, China  
KANG JianFei Inner Mongolia No.8 Geological and Mineral Exploration and Development Co. Ltd., Wuhai 016000, Inner Mongolia, China  
BAI Tao Inner Mongolia Mining Development Co. Ltd., Hohhot 010011, Inner Mongolia, China  
ZHOU LiJun Inner Mongolia Geology and Mineral Resources(Group) Co., Ltd., Hohhot 010011, Inner Mongolia, China  
基金项目:本文得到内蒙古自治区地质勘查基金管理中心项目(编号:11-1-KC11)资助
中文摘要:复兴屯银铅锌矿床位于大兴安岭南段中生代宝石火山沉积盆地内,是内蒙古近年来地质找矿的一大突破。文章通过分析复兴屯区域地质背景及矿床地质特征,详细介绍了地球物理及地球化学在该矿床找矿过程中的应用,最后总结了矿床的找矿标志。复兴屯银铅锌矿体产于晚侏罗世—早白垩世陆相火山碎屑岩内,其形态、规模、产状受火山机构-网格状断裂构造体系控制,呈“拱形”产出。矿床以独立银矿体、银铅锌共生矿体为主,其次为锌矿体、铅矿体、锌铅矿体,均为隐伏矿体。矿体形态为似层状、透镜状,主要矿化蚀变有叶腊石化、绿泥石化、高岭土化、碳酸盐化、菱锰矿化、闪锌矿化、方铅矿、黄铁矿化,局部见黄铜矿化。该矿床推断Ag金属资源量5258 t,平均品位198.21 g/t;Zn金属推断资源量17.6万t,平均品位1.61%;Pb金属推断资源量3.3万t,平均品位1.36%,达超大型规模。文章初步总结出复兴屯矿床找矿标志:晚侏罗世—早白垩世陆相火山碎屑岩、网格状断裂构造体系、破火山口和火山盆地、矿化蚀变(铁锰碳酸盐化、硅化、叶腊石化、黄铁矿化、铅锌矿化)、平面及垂向Ag-Pb-Zn-CuAu元素异常组合、环状平稳负磁异常和低阻高极化激电异常。复兴屯超大型银铅锌矿床地质特征及找矿标志的研究为大兴安岭地区类似矿床提供找矿思路,同时也为该区寻找隐伏矿体提供一种有效的勘查模型。
中文关键词:地质特征  找矿标志  银铅锌矿床  复兴屯  大兴安岭南段
 
Geological characteristics and prospecting indicators of Fuxingtun giant Ag-Pb-Zn deposit in Inner Mongolia
Abstract:The giant Fuxingtun Ag-Pb-Zn deposit is located in the Mesozoic Baoshi volcanic-sedimentary basin of the southern Da Hinggan Mountains. The discovery of this deposit is a major breakthrough in geological prospecting in Inner Mongolia in recent years. The orebodies of the deposit occur within the Late Jurassic-Early Cretaceous continental pyroclastic rock and are controlled by both the volcanic mechanism and grid fault structural system. The inferred resource of Ag metal is 5258 t with an average grade of 198.21g/t, the inferred resource of Zn metal is 1.76 hundred thousand tons with an average grade of 1.61%, and the inferred resource of Pb metal is 0.33 hundred thousand tons with an average grade of 1.36%. Based on the analyses of the regional geological setting and geological characteristics of the Fuxingtun deposit, it is preliminarily considered that the prospecting indicators of this type of deposit are as follows: ① Late Jurassic-Early Cretaceous continental pyroclastic rocks; ② grid fault structural system; ③ caldera and volcanic basin; ④ Fe-Mn carbonation, silicification, pyrophrllitization, pyritization, Pb-Zn mineralization; ⑤ Ag-Pb-Zn-Cu-Au element anomaly combinations; ⑥annular stable negative magnetic anomaly; and ⑦ low resistance and high induced polarization anomaly. Through the study on the geological characteristics and prospecting indicators of the Fuxingtun deposit, this paper aims to provide prospecting ideas for similar deposits in the Da Hinggan Mountains and also provide an effective exploration model for finding concealed ore bodies in this area.
keywords:geological characteristics  prospecting indicators  Ag-Pb-Zn deposit  Fuxingtun  southern Da Hinggan Mountains
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