安徽池州西山钼矿地物化特征及矿床成因分析  

Analysis of physicochemical characteristics and genesis of the molybdenum deposit in Xishan,Chizhou,Anhui

作　　者：伍佳杰 方梅[1] WU Jiajie;FANG Mei(No.324 Unit of Bureau of Geology and Mineral Exploration of Anhui Province,Chizhou 247100,Anhui,China;China University of Geosciences(Wuhan),Wuhan 430074,Hubei,China)

机构地区：[1]安徽省地质矿产勘查局324地质队,安徽池州247100 [2]中国地质大学(武汉),湖北武汉430074

出　　处：《资源信息与工程》2022年第1期31-33,36,共4页Resource Information and Engineering

基　　金：安徽省地质勘查基金项目“安徽省池州市西山钼矿普查(2009-1-25)”。

摘　　要：安徽省池州市西山钼矿区域构造位于贵池背向斜带之灌口—潘桥向斜南东翼中段,北东向高坦深断裂与北北东向马头断裂交汇处。矿区内主矿体主要赋存在岩体与围岩接触带及外侧围岩(强绢英岩化带)中,受岩体与围岩接触带及北东向含矿裂隙带控制,具有良好的钼矿成矿条件。文章对研究区的地质、地球物理及地球化学特征进行多元化信息归纳,同时分析矿床成因,为后期进一步找矿提供依据。The regional structure of Xishan molybdenum mine in Chizhou City,Anhui Province is located in the middle section of the southeast wing of Guankou Panqiao Syncline in Guichi back syncline,at the intersection of northeast Gaotan deep fault and northeast Matou fault.The main ore body in the mining area is mainly located in the contact zone between rock mass and surrounding rock and the outer surrounding rock(strong sericitization zone),which is controlled by the contact zone between rock mass and surrounding rock and the ne ore bearing fracture zone,and has good molybdenum ore⁃forming conditions.This paper summarized the geological,geophysical and geochemical characteristics of the study area,and analyzed the genesis of the deposit,which provided a basis for further prospecting.

关 键 词：地质特征 地球物理特征 地球化学特征 矿床成因 西山钼矿区 

分 类 号：P618[天文地球—矿床学]