岩浆岩及与之有关的内生矿化的地球化学是现代地球化学的一个主要研究方面。它把岩石的成因、岩浆源的潜在含矿性和成矿率以及金属元素和稀有元素在岩浆和岩浆期后作用过程中的地球化学历史等问题,有机地结合在一起。 在这方面的一个十分重要的研究成果,就是利用岩石-地球化学资料能作成矿分析。现今获得的关于岩浆中稀有元素和金属元素的大量地球化学资料,已能够十分有把握地从这些岩石的岩体中区分出潜在含矿性的岩体;根据这些侵入体侵入时形成的火山深成系统的构造形态特征,可以预测地球化学富集场的分 Magmatic rocks and their associated endogenous mineralization geochemistry is a major research area of ​​modern geochemistry. It organically combines the causes of rock, the potential mineralization and the mineralization rate of magmatic source, and the geochemical history of metal elements and rare elements during the magmatic and post-magmatic periods. A very important research in this area is the use of rock-geochemical data for mineral analysis. The large amount of geochemical data available today on the rare and magmatic elements of the magma have been able to distinguish the potentially ore-bearing rock mass from the rock mass of these rocks with great certainty. Based on the volcanic depth Into the system of structural features, can predict the geochemical enrichment field points