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有些文献对与火山深成岩发育地区有空间联系的铀钼矿床形成的地质-构造特征,矿石矿物成分作过详细的介绍。个别人对古火山机体中铀钼矿床矿化分带性的特点进行过研究,证明铀矿化与钼矿化在空间上是分开的。但是,文献中缺少有关铀少钼多为特征的热液矿化分布特点方面的资料。既然把铀矿石中存在钼视作找铀的直接找矿标志,那么对火山深成建造中这种类型矿床分布特征的研究,就很重要了。
Some documents provide a detailed introduction to the geologic-tectonic features and mineral composition of uranium-molybdenum deposits that have spatial connection with volcanic plutons. Someone studied the characteristics of mineralization and zonation of uranium-molybdenum deposits in ancient volcanic bodies, proving that uranium mineralization and molybdenum mineralization are spatially separated. However, the literature lacks data on the distribution characteristics of hydrothermal mineralization characterized by less molybdenum and uranium. Since the presence of molybdenum in uranium ore is considered as a direct prospecting symbol for finding uranium, it is important to study the distribution characteristics of this type of deposit in the deep volcanic erection.