内蒙古阿吉勒银铅锌多金属矿床控矿条件及找矿方向分析  

Ore Controlling Factors and Prospecting for Ajile SilverLead-Zinc Polymetallic Deposit in Inner Mongolia

作　　者：徐桓[1] 李翾[1] 王志民[1] 秦越强 王末[1] 冯欣[1] 祝小松 

机构地区：[1]武警黄金第四支队,辽宁辽阳111000

出　　处：《甘肃冶金》2014年第2期66-70,共5页Gansu Metallurgy

摘　　要：阿吉勒银铅锌多金属矿为新近发现的有找矿前景的一处普查区。矿区位于华北板块与西伯利亚板块缝合带的北侧。距阿尔哈达铅锌矿110 km。铅锌矿脉主要赋存于石炭系-二叠系火山碎屑岩中,该地层提供了矿源层;受NW向断裂构造控制,构造提供了矿化进一步富集的动力条件,使矿质得以活化、迁移并在有利成矿空间定位形成矿体。本文通过对控矿因素进行了分析,指明了下步找矿方向。The perspective Ajile silver-Lead-Zinc polymetallic deposit has been put forward to the study area lately , located in north part of the north China plate and Siberia plate suture zone , about 110km from the Arhada Lead Zinc deposit .The lead-zinc ore occurs mainly in volcaniclastic rock of Caboniferous-Permian.Ore-bearing layers offered metal source .The de-posit was structurally controlled by north-west fracture structure and the structure offered dynamic force for ore forming , which made the ore-forming source activated , transferred and deposited in favorable location .Through analysis of major ore controlling factors , further prospecting direction is indicated .

关 键 词：铅锌多金属矿 控矿因素 找矿方向 阿吉勒 内蒙古 

分 类 号：P612[天文地球—矿床学]