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江西省大地热流与铀矿关系的初步研究
引用本文:李学礼,周文斌,张卫民,孙占学.江西省大地热流与铀矿关系的初步研究[J].铀矿地质,1993(4).
作者姓名:李学礼  周文斌  张卫民  孙占学
作者单位:华东地质学院,华东地质学院,华东地质学院,华东地质学院 江西抚州 344000,江西抚州 344000,江西抚州 344000,江西抚州 344000
摘    要:本文根据江西省大地构造、铀矿分布和大地热流实测资料,证明大地热流异常和铀矿均受深大断裂和深部构造变异带的控制,铀矿化能在一定程度上引起热流异常,并据此初步探讨了根据大地热流异常寻找铀矿床的可能性。

关 键 词:大地热流  大地构造  地热异常  铀矿

RELATION BETWEEN TERRESTRIAL HEAT FLOW AND URANIUM DEPOSITS IN JIANGXI PROVINCE
Li Xueli Zhou Wenbin ZhangWeimin Sun Zhanxue.RELATION BETWEEN TERRESTRIAL HEAT FLOW AND URANIUM DEPOSITS IN JIANGXI PROVINCE[J].Uranium Geology,1993(4).
Authors:Li Xueli Zhou Wenbin ZhangWeimin Sun Zhanxue
Abstract:Based on tectonic features,distribution of uranium deposits and terrestrial heat folw data,this paper reveals that heat flow anomaly and urahium mineralization are controlled by deep-seated faults and deep-seated structural transitional zones. To some extent, uranium mineralization can cause heat flow anomalies. Possibilities of prospecting for uranium by heat flow measurement method is preliminarily discussed in this paper as well.
Keywords:Terrestrial Heat Flow  Tectonic features  Heat flow anomaly  Uranium deposit  
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