摘要
302铀矿床是一个垂幅大、垂直分带较完整的花岗岩型铀矿床。研究结果表明,热液脉体在垂向上表现出“上酸下碱、上氧化下还原”的分带性。这一垂直分带的主要原因是热液的混合和沸腾作用。
The No. 302 uranium deposit is a granite type deposit with considerable vertical extension and relatively complete vertical zoning. Studies of hydrothermal dikes reveal the existence of vertical zoning characterized by 'acid and oxidized minerals present in the upper part, and alkaline and reduced minerals seen in the lower part', which is believed to have resulted from the mixing and boiling of hydrothermal solutions.
出处
《矿床地质》
CAS
CSCD
北大核心
1992年第3期252-258,共7页
Mineral Deposits
