铀成矿带是地质学中的术语,是指具有共同地质构造特征和成因联系的铀矿田或铀矿床组合的分布地带。
粤北铀矿区是南岭铀成矿带核心地段,也是我国花岗岩型铀矿首先突破、集中发育地区。
The northern Guangdong uranium metallogenic region is the central part of Nanling uranium metallogenic belt.
从成矿地质条件分析,武夷火山铀成矿带中的主要铀矿床的共同点是都具有花岗岩基底岩石。
The analysis of ore forming conditions suggests a common point in the main uranium deposits of Wuyi volcanic uranium mineralization belt that they all have granite as the basement rokes.
但由于该区的层间氧化带形成的时代较新,且成矿的铀源条件相对较差,因此,该区黄色层间氧化带的成矿前景还需进一步探索。
Due to the young age of interlayer oxidation and unsatisfied uranium sources, uranium metallogenic prospect of this area need more research and exploration.
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