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广西苗儿山地区马家铀矿床成矿地质特征研究

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广西马家铀矿床为花岗岩型铀矿,在新一轮铀矿地质勘查工作中取得了较好的找矿成果.不同于区内其他铀矿床赋存在印支期岩体中,马家铀矿床赋存在加里东期岩体内,是在加里东期岩体中铀矿找矿的新突破.从赋矿围岩、控矿构造、围岩蚀变和铀矿化等方面分析了马家铀矿床的成矿地质特征,认为区内铀源丰富,加里东期岩体为产铀岩体;NNE向断裂构造规模大,其次级成矿构造发育,铀矿体严格受F2709、F2715和F2719等含矿断裂带控制;热液蚀变作用强烈,赤铁矿化、碳酸盐化、硅化、钾长石化、紫黑色萤石化与铀矿化关系密切;控矿因素主要为富铀花岗岩、断裂构造和热液蚀变.下一步的勘查工作需加强在苗儿山岩体及相邻越城岭岩体中寻找同类型铀矿,继续加强对F2719、F2715和F2709等含矿断裂带的勘查力度,开展深部地质勘查,寻找富大铀矿体,扩大矿床资源量.
Study on geological features of Majia uranium deposit in Guangxi province
Majia uranium deposit in Guangxi is a granite type uranium deposit founded in the new round of uranium geologic exploration.The deposit is hosted in the Caledonian pluton,which is different from other uranium deposits in the area and indicate the uranium prospecting breakthrough in the Caledonian pluton.To summarize the characteristics of this kind of deposit,the author analyzed the uranium metallogenic geological characteristics in the host rock,ore-controlling structure,wall-rock alteration and uranium mineralization and had came to the following conclusions:there are abundant uranium sources in the area,and Caledonian granite acted as the uranium producing pluton.The NNE trending fault in the area is large in scale and derived rich secondary structure which controlled the uranium ore body strictly as by F2709,F2715,F2719 ore-bearing fault zone,hydrothermal alterations are strongly developed as hematitization,carbonatization,silication,K feldsparization and fluoritization,which are closely related to the uranium mineralization.It is believed that uranium deposits is mainly controlled by U-rich granite,faults and hydrothermal alterations.The next exploration should be oriented in finding the same type uranium deposit in Miaoershan and Yuechengling plutons,and continue to explore along F2709,F2715,F2719 ore-bearing fault zone,and strengthen the exploration in the depth for large and rich uranium ore bodies.

metallogenic characteristicsgranite type uranium depositCaledonian graniteMajia uranium deposit

郑可志、陈东欢、庞雅庆、罗桥花、肖为

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广西三一〇核地质大队,广西 桂林 541213

中国铀业纳米比亚矿业有限公司,纳米比亚 斯瓦科普蒙德 8350

核工业北京地质研究院 中核集团铀资源勘查与评价技术重点实验室,北京 100029

北京市地质调查研究所,北京 100195

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成矿地质特征 花岗岩型铀矿 加里东期岩体 马家铀矿床

广西壮族自治区找矿突破战略行动地质矿产勘查项目

桂国土资函[2017]547号

2024

世界核地质科学
核工业北京地质研究院

世界核地质科学

CSTPCD
影响因子:0.463
ISSN:1672-0636
年,卷(期):2024.41(3)
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