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.
出处
《资源环境与工程》
2013年第3期249-251,共3页
Resources Environment & Engineering
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
Niutitang formation
lithology
sturcure
interlayer fracture zone
redox zone
uranium ore body
controlling factors
