摘要
鲍家火山盆地铀矿化受构造、岩层双重控制,并与金属硫化物密切相关。盆地内岩矿石电性差异明显。测量显示,铀矿化地段呈高极化率(sη)、低电阻率(sρ),异常特征峰显著,与深部铀矿化对应良好,对该地区铀矿勘查具有指示意义和良好的应用前景。
In Baojia volcanic basin uranium mineralization is controlled by structure and rock formation, and closely related to metallic mineral of sulfide. There is great difference of electric property between uranium ore rock and adjoining rock. Electrical sounding show that high potarizability （ηs） and low resistivity （ρs） peak notable of potarizability are characteristics of uranium mineralization which correspondence to underground uranium mineralization. This method can be used to guide uranium exploration in this area.
出处
《铀矿地质》
CAS
CSCD
2006年第6期361-367,共7页
Uranium Geology
关键词
铀矿化
金属硫化物
激电异常
鲍家火山盆地
uranium mineralization
metallic mineral of sulfide
potarizability
Baojia volcanic basin
