华北地区锡矿成矿规律及找矿方向  

Metallogenic regularity and prospecting direction of Tin deposits in North China

作　　者：田杰鹏 李俊建[4] 张彤[5] 付超 党智财 何江涛 张鹏鹏 TIAN Jie-peng;LI Jun-jian;ZHANG Tong;FU Chao;DANG Zhi-cai;HE Jiang-tao;ZHANG Peng-peng(Key Laboratory of Building Structural Retrofitting and Underground Space Engineering of Ministry of Education,Jinan 250101,China;School of Civil Engineering,Shandong Jianzhu University,Jinan 250101,China;Key Laboratory of Gold Mineralization Processes and Resource Utilization Subordinated to the Ministry of Land and Resources,Key Laboratory of Metallogenic Geological Process and Resources Utilization in Shandong Province,Jinan 250013,China;Tianjin Center,China Geological Survey,Tianjin 300170,China;Geological Survey Institute of Inner Mongolia Autonomous Region,Hohhot 050081,China;Institute of Geophysical and Geochemical Exploration of Chinese Academy of Geological Science,Langfang 065000,China;Hebei GEO University,Shijiazhuang 050031,China)

机构地区：[1]建筑结构加固改造与地下空间工程教育部重点实验室,济南250101 [2]山东建筑大学土木工程学院,济南250101 [3]自然资源部金矿成矿过程与资源利用重点实验室,山东省金属矿产成矿地质过程与资源利用重点实验室,济南250013 [4]中国地质调查局天津地质调查中心,天津300170 [5]内蒙古自治区地质调查院,呼和浩特010020 [6]中国地质科学院地球物理地球化学勘查研究所,河北廊坊065000 [7]河北地质大学,石家庄050031

出　　处：《华北地质》2023年第1期20-26,共7页North China Geology

基　　金：中国地质调查局项目“华北地区区域成矿规律研究与总结(DD20190379-31)”;“华北地区矿产资源潜力评价(1212011121029)”;“华北地台成矿规律研究和找矿方向综合研究(200110200038)”;“国家重点研发计划深地资源勘查开采重点专项胶东矿集区三维结构与定位预测课题(2016YFC0600107)”;“胶东招平带北段金矿深部预测与勘查示范专题(2018YFC0603805-1)”。

摘　　要：我国华北地区锡矿资源较为丰富,尤其是大兴安岭中南段,是我国三大主要锡成矿区之一,也是我国北方目前发现的唯一一个成型的锡多金属矿带。华北地区锡矿床类型主要分为热液型、斑岩型和接触交代型三类,多数为共生和伴生矿床,独立锡矿床较少。区内锡矿床成矿期主要集中于晚侏罗-早白垩世。本文分析了华北地区锡矿的主要控矿因素,初步建立了接触交代型、斑岩型和热液型锡矿床的成矿模式,探讨了锡矿的时空分布规律,提出锡林浩特-克什克腾旗、二连-东乌旗及商都-太仆寺旗地区为华北地区寻找锡矿的重点地区。Tin resources are abundant in North China,especially in the middle and southern Greater Khingan Range,which is one of the three major tin mining areas in our country and the only formed tin polymetallic ore belt found in the north of China.The types of tin deposits in North China are mainly divided into three categories:hydrothermal,porphyry and contact account type,most of which are co-occurring and associated deposits,with few independent tin deposits.The mineralization period of tin deposits in the region is mainly concentrated in the Late Jurassic-Early Cretaceous.On this basis,the main ore-controlling factors of tin deposits in North China were analyzed,the metallogenic models of contact metasomatic,porphyry and hydrothermal tin deposits were initially established,and the temporal and spatial distribution of tin deposits were discussed,and Xilinhot-Keshiketeng Banner,Erlian-Dongwu Banner and Shangdu-Taipusi Banner are key areas for searching for tin deposits in North China.

关 键 词：接触交代型 热液型 斑岩型 成矿模式 找矿方向 锡矿 华北地区 

分 类 号：P618.44[天文地球—矿床学]