首页|内蒙古霍布林查干铅锌银多金属矿床地质特征及找矿前景

内蒙古霍布林查干铅锌银多金属矿床地质特征及找矿前景

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霍布林查干铅锌银多金属矿床位于内蒙古东乌珠穆沁旗东部,构造属兴蒙造山带中部、大兴安岭成矿带西侧.为研究矿区成矿背景及找矿潜力,在矿区采用 1∶10 000 地质填图、土壤化探测量、激电测量、槽探和钻探工程等方法开展地质勘查及研究工作,并对矿区地质特征、矿床地质特征及成因进行了详细探讨.研究表明:① 霍布林查干铅锌银多金属矿为构造热液型矿床,容矿地层为侏罗系玛尼吐组和白垩系白音高老组;② 矿化带赋存于NW向断层F1、F3 内,其中,S1 矿化带圈定了 8 条矿体,S2 矿化带圈定了 2 条矿体,矿体在空间上成脉状大致平行排列,合计铅锌资源量达中型规模;③ 矿石由闪锌矿、方铅矿组成,矿石结构、构造类型多样;④ 矿床与物化探异常关系密切,成矿范围内铅锌银元素往往浓集中心明显,异常发育中带、内带,激电呈高极化率、低电阻率特征.在上述分析的基础上,结合矿床地质特征、地球物理特征、找矿标志等,分析了区域找矿前景,并初步圈定了 4 处找矿靶区,认为各靶区成矿潜力均较好,值得进一步开展工作.该矿床的发现弥补了满都宝力格—红旗村一带金属矿空白,充分说明在朝不楞—乌拉盖断裂带(F5)以东地区仍具有非常大的找矿潜力.
Geological Characteristics and Prospecting Potential of Huobulin Pb-Zn-Ag Polymetallic Deposit in Inner Mongolia
Huobulinchagan Pb-Zn-Ag polymetallic ore deposit is located in the east of East Ujumuqin Banner,Inner Mongolia.The structure belongs to the middle part of Xingmeng orogenic belt and west side of the Great Xing'an Mountains metallogenic belt.In order to study the background of mineralization and exploration potential in the mining area,by means of 1∶10 000 geological survey,soil geochemical survey,IP survey,trench engineering and drilling engineering,the regional metal-logenic geological background,geological characteristics of the mining are analyzed and deposit genesis of the mining area are studied comprehensively.The study results show that:① Huobulinchagan Pb-Zn-Ag Polymetallic ore deposit is structural hy-drothermal lead-zinc deposit and the host strata of Huobulinchagan Pb-Zn-Ag Polymetallic ore deposit are Jura Manitu Group and the Cretaceous Baiyigaolao Group.② The mineralized zone is hosted in the northwest faults F1 and F3,with 8 mineralized bodies in S1 and 2 mineralized bodies in S2.These mineralized bodies are approximately parallel to each other and in the form of vein in space.③ The ore consists of sphalerite and galenawith various types of ore texture and structure.④ The relationship between the mineral deposit and geophysical and geochemical anomalies is close,and the centers of concentration of lead,zinc and silver elements within the metallogenic range are often obvious with middle and inner zones of anomalies.The IP shows high polarizability and low resistivity characteristics.Based on the discussion results,combing with the geological characteristics and geophysical characteristics of the mining area and prospecting criteria of the area,the prospecting model of sedimentary i-ron deposit is established,four prospecting target areas are delineated,the further discussion results indicated that prospecting potential of the target areas are good.In summary,the discovery of this deposit fills the gap in metal deposits in the area from Mandubolixilai to Hongqichun,which fully demonstrates that there is great potential for mineral exploration in the area east of the Chaobuleng West-Wulagai fault(F5).

Pb-Zn-Ag polymetallic depositdeposit geological characteristicsgenesis of depositprospecting potentialprospecting target area

王世权、任利平、胡红雷、陈俊魁、吕宪河、李东

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河南省地质研究院,河南 郑州 450001

河南省地质局矿产资源勘查中心,河南 郑州 450001

铅锌银多金属矿床 矿床地质特征 矿床成因 找矿前景 找矿靶区

内蒙古自治区地质勘查基金项目河南省地质研究院项目

11-2-KC892023-903-KT01

2024

金属矿山
中钢集团马鞍山矿山研究院 中国金属学会

金属矿山

CSTPCD北大核心
影响因子:0.935
ISSN:1001-1250
年,卷(期):2024.(6)