湖北省崇阳县梯冲铀矿床成矿控制因素探讨  

Discussion on Ore-controlling Factors of Tichong Uranium Deposit in Chongyang County,Hubei Province

作　　者：刘艳 

机构地区：[1]湖北省核工业地质局,湖北孝感432000

出　　处：《资源环境与工程》2013年第3期249-251,共3页Resources Environment & Engineering

摘　　要：对崇阳梯冲铀矿床从区域地质背景、含矿地层、岩性与区域构造和含矿构造关系进行探讨。确立了铀矿床受层位、岩性层间破碎带及氧化还原带等因素控制,即矿床产于寒武系下统牛蹄塘组黑色岩系之中,矿体赋存于近东西向层间挤压破碎带之中,并受氧化还原界面制约的成矿规律。对寻找同类型铀矿床有一定的指导意义。In this paper the author discusses Tichong uranium deposit from regional geological bakground,ore-bearing strata,lithology and relationship between regional tectonic and ore-bearing structure,establishes uranium deposit is controlled by some factors such as layers,lithology interlayer fracture zone and redox zone.It is helpful for looking for the same type of uranium deposits.

关 键 词：牛蹄塘组 岩性 构造 层间破碎带 氧化还原带 铀矿体 控制因素 

分 类 号：P619.14[天文地球—矿床学]