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关于与钼矿床所有基本成因类型有关的花岗岩中钼的地球化学问题,许多研究者已作过讨论。尽管如此,但是对于这一问题尚有许多不清楚之处,特别是在不同岩石类型中钼的含量、成因上有联系的岩石和矿物系列中钼的分布特征以及钼的赋存形式等方面。这就有碍于建立内生钼矿床的形成模式和确立它们预测的科学依据。笔者获得的新的研究成果,可在一定程度上解决这些问题。现已发表的有关花岗岩中钼含量的资料很不一致,测定值也很分散,从>0.13到7.7克/吨,多数在1.5克/吨左右。据П.Курода和Э.Сандел(1959)报道,
Many researchers have discussed the geochemistry of molybdenum in granites associated with all the basic genetic types of molybdenum deposits. Nevertheless, there are many uncertainties about this issue, especially in terms of molybdenum content in different rock types, genetically linked distribution characteristics of molybdenum in the rock and mineral series, and the occurrence of molybdenum. This hindered the establishment of endogenous molybdenum deposit formation patterns and establish their scientific predictions. The author’s new research results, to some extent, can solve these problems. The published data on molybdenum content in granite are very inconsistent and the measured values are also very scattered, from> 0.13 to 7.7 g / t, mostly at about 1.5 g / t. According to reports by П.Курода and Э.Сандел (1959)