首页|广西摩天岭地区达亮铀矿床地质特征及找矿标志

广西摩天岭地区达亮铀矿床地质特征及找矿标志

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达亮铀矿床产于摩天岭岩体西南缘与四堡群沉积变质岩系之内外接触带0.5~1 km范围内,是华南地区热液型铀矿成矿时代最早的矿床之一.为进一步分析达亮地区铀矿成矿物源及其成矿约束条件,还原成矿过程,明晰勘查找矿标志,文章在总结矿床地质特征的基础上,针对控矿因素、微量元素与稀土元素地球化学特征等方面进行了探讨.研究结果表明,达亮铀矿床围岩铀浸出率高,矿体受断裂约束明显,与铀元素活化、迁移、富集密切相关的有Sb、Y、W、Pb、Sr、Nb、Ba等微量元素,矿石微量元素变化规律与围岩具有相似性.铀矿石Y/Ho值为37.33~45.60,高于围岩Y/Ho值24.83~29.68,两者稀土配分模式差异较大.综合分析认为达亮地区铀矿成矿物质并非完全来自围岩地层及摩天岭花岗岩,还有来自成矿期的深源物质参与.
Geological characteristics and prospecting indicator of Daliang uranium deposit in Motianling area,Guangxi
Daliang uranium deposit is located within the 0.5-1 km range of the inner and outer contact zone between the southwest edge of Motianling rock mass and the sedimentary metamorphic rock series of Sibao Group.It is one of the earliest mineralization age uranium deposits in South China.In order to further re-store the uranium mineralization process in Daliang area and to determine the exploration and prospecting in-dicator,this article has discussed various aspects such as geological characteristics of the deposit,orebody characteristics,ore-controlling factor,and geochemical characteristics of trace elements and rare earth ele-ments.The research result indicates that the uranium leaching rate of the surrounding rock in Daliang urani-um deposit is high,and the orebody is significantly controlled by the fault structures.Trace elements such as Sb,Y,W,Pb,Sr,Nb,Ba are closely related to the activation,migration and enrichment of U element.The variation pattern of trace elements in the ore is similar to that of the surrounding rock.The Y/Ho value of uranium ore is 37.33-45.60,which is higher than the Y/Ho value of surrounding rock,which is 24.83-29.68.There is a significant difference in the REE distribution pattern between them.Based on the comprehen-sive analysis,it is considered that the ore-forming materials in Daliang area are not entirely derived from the surrounding rocks,and the deep source materials are also involved.

Motianling granite massDaliang deposituranium mineralization featureprospecting mark

麻乾坤、庞雅庆、刘明、文成、范鹏飞

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核工业二三○研究所,湖南长沙 410007

核工业北京地质研究院,北京 100029

摩天岭花岗岩体 达亮矿床 铀矿化特征 找矿标志

中国核工业地质局

202238-10/202223-8

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(1)
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