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下庄铀矿田及外围深部找矿的地质依据
引用本文:冯志军,黄宏坤,曾文伟,吴继光.下庄铀矿田及外围深部找矿的地质依据[J].铀矿地质,2011,27(4):221-224.
作者姓名:冯志军  黄宏坤  曾文伟  吴继光
作者单位:广东省核工业地质局293大队,广东广州,510800
摘    要:通过对下庄花岗岩型铀矿田深断裂的控矿作用、成矿物质和成矿流体的物质来源、辉绿岩与硅化带的空间关系,以及普通物探成果和钻孔揭露情况等的研究,展望了下庄矿田深部找矿的潜力。

关 键 词:花岗岩型铀矿田  成矿物质  成矿流体  深部找矿

Geological evidence for deep exploration in Xiazhuang uranium orefield and its periphery
FENG Zhi-jun,HUANG Hong-kun,ZEN Wen-wei,WU Ji-guang.Geological evidence for deep exploration in Xiazhuang uranium orefield and its periphery[J].Uranium Geology,2011,27(4):221-224.
Authors:FENG Zhi-jun  HUANG Hong-kun  ZEN Wen-wei  WU Ji-guang
Institution:FENG Zhi-jun,HUANG Hong-kun,ZEN Wen-wei,WU Ji-guang(Party No.293,Geological Bureau for Nuclear Industry of Guangdong,Guangzhou,Guangdong 510800,China)
Abstract:This paper first discussed the ore-controlling role of deep structre,the origin of metallogenic matter and fluid,the relation of diabase to silicification zone,then summarized the achievement of Geophysical survey and drilling,and finaly analysed the potential for deep exploration in Xiazhuang uranium orefield.
Keywords:granite-type uranium orefield  metallogenic matter  merallogenic fluid  deep exploration  
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