首页|大兴安岭南段乌苏图如地区锡多金属矿地质特征及找矿潜力

大兴安岭南段乌苏图如地区锡多金属矿地质特征及找矿潜力

Geological Characteristics and Prospecting Potential of Tin Polymetallic Deposit in the Wusuturu Area,Southern Da Hinggan Mountains

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大兴安岭地区是我国重要的锡成矿带之一,乌苏图如地区位于大兴安岭南段,西伯利亚板块和华北板块之间的增生造山带上,属突泉—林西华力西、燕山期铁(锡)、铜、铅、锌、银、铌钽三级成矿带.为查明该区成矿规律及找矿潜力,通过综合开展 1∶5 万矿产地质调查、1∶5 万水系沉积物测量、1∶5 万高精度磁测及 1∶1 万地质草测、1∶2.5万土壤测量、1∶1 万地化剖面测量、1∶1 万激电中梯剖面测量、激电测深、槽探等工作,对区域成矿地质特征及成矿潜力进行了研究.结果表明:① 区内以锡、铅、锌、铜、银等内生金属矿为主,新发现矿(化)点 21 处;② 1∶5 万水系沉积物测量圈出化探单元素异常 438 个,综合异常 57 个;③ 1∶5 万高精度磁测圈定规模较大的磁异常 34 个,区内矿(化)点多处于正磁异常区与负磁异常区之间的梯度带上,是寻找多金属矿的有利部位;④ 矿床成因类型为热液型和接触交代型,主要成矿期为华力西成矿期和燕山成矿期,燕山期为锡多金属矿的主要成矿期;⑤ 区内矿产分布严格受控于地质构造、岩体以及地层,在横向分布上呈NE向带状展布,由北向南共5 个矿带;⑥ 提交各类找矿靶区16 处,其中以锡为主要矿种或伴生矿种的找矿靶区 7 个.
Da Hinggan Mountains area is one of the most important tin metallogenic belts in China,and the Wusuturu ar-ea is located in the south of the Da Hinggan Mountains,on the accretionary orogenic belt between the Siberian Plate and the North China Plate,belonging to the Tuquan-Linxi Hualixi period and Yanshan period iron(tin),copper,lead,zinc,silver,nio-bium-tantalum metallogenic belt.In order to find out the metallogenic regularity and prospecting potential of this area,by com-prehensively carrying out 1∶50000 mineral geological survey,1∶50000 stream sediment survey,1∶50000 high-precision mag-netic survey and 1∶25000 soil survey,1∶10000 geological grass survey,1∶10000 geochemical profile survey,1∶10000 IP mid-ladder profile survey,IP sounding,trenching and other working methods,the metallogenic geological characteristics and metallogenic potential are studied.The results show that:① The area is dominated by endogenous metal deposits such as tin,lead,zinc,copper and silver,and 21 new ore(mineralization)points have been discovered;② There are 438 geochemical sin-gle element anomalies and 57 comprehensive anomalies by 1∶50000 stream sediment survey;③ 34 large scale magnetic anom-alies were delineated by 1∶50000 high-precision magnetic survey,and most of the mineralization points in the area were in the gradient belt between the positive and negative magnetic anomalies,which was a favorable location for searching for polymetal-lic ore;④ The genetic types of the deposit are hydrothermal type and contact metasomatism type,the main mineralization peri-ods are Hualixi mineralization period and Yanshan mineralization period,and Yanshan mineralization period is the main miner-alization period of tin polymetallic deposit;⑤ The distribution of mineral resources is strictly controlled by geological structure,rock mass and strata,and the horizontal distribution is distributed in a band to northeast,with a total of 5 ore belts from north to south;⑥ 16 prospecting targets of various types were submitted,including 7 prospecting targets with tin as the main mineral or associated mineral.

tin polymetallicgeophysical explorationgeochemical explorationmetallogenic regularityprospecting potential

闫红圃、李瑞强、刘文毅、孙国峰、张得恩、张沁妍

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河南省地质研究院,河南 郑州 450016

河南省金属矿产成矿地质过程与资源利用重点实验室,河南 郑州 450016

河南省金属矿产深部控矿与成矿机制院士工作站,河南 郑州 450016

锡多金属矿 地球物理 地球化学 成矿规律 找矿潜力

2023年度河南省自然资源科研项目内蒙古地质勘查基金项目

2023-382-1405-5-KD09

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.(8)