近年来,发现了贝尼奥夫-查瓦里茨基带的巨大控矿作用以及与该带有关的侧向岩浆和成矿分带。 研究哈萨克斯坦花岗岩类的经验表明,在同一时代的花岗岩类岩石中,岩石的总碱度和钠碱度随着离岩石圈板块假想界面向大陆深部的递增,而且岩石的基性度也随之增长。这就造成了按碱度-基性度划分花岗岩岩石化学类型及与之有关的内生矿化的带状分布。特别要强调的是,含斜长花岗闪长岩和石英闪长 In recent years, the great ore-controlling effect of the Benioff-Charivalitz base band and the lateral magmatic and metallogenic belts associated with the belt have been discovered. The study of granite in Kazakhstan shows that in the granitic rocks of the same age, the total alkalinity and sodium basicity of the rock increase with the depth from the hypothetical interface of the lithospheric plate to the continental margin, and the basicity of the rock also follows increase. This resulted in the classification of granitoids based on alkalinity and basicity, and the associated belt-like distribution of endogenous mineralization. Special emphasis should be on the inclusion of plagiogranite and quartz diorite