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。
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.
出处
《铀矿地质》
CAS
CSCD
北大核心
1993年第4期22-26,共5页
Uranium Geology
基金
国家自然科学基金
关键词
大地热流
大地构造
地热异常
铀矿
Terrestrial Heat Flow, Tectonic features, Heat flow anomaly, Uranium deposit
