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在一定的条件下,岩浆岩、沉积岩和变质岩建造可成为矿质的来源.由此而得出的矿化与地球深部构造的联系,大体上已在理论上得到证实,或被一些地区的经验所肯定.作者于1968～1972年间研究了阿尔泰-萨扬地区的矿床与相当于成矿区、矿田、矿结规模的地壳局部非均匀性之间的关系,编制了地壳层的厚度图,查明了389个铜、锌、铅、银、钼和钨矿床及2050个矿点相对于每一地壳层及其比值的分布.
Under certain conditions, the formation of magmatic rocks, sedimentary rocks and metamorphic rocks can become a source of mineralization, and the resulting mineralization has been largely confirmed in theory by the deep experience of the earth’s deep structure The author from 1968 to 1972 studied the Altai-Sayan area of the deposit and the equivalent of metallogenetic area, ore field, scale of the crustal local non-uniform relationship between the preparation of the crust thickness map, check The distribution of 389 copper, zinc, lead, silver, molybdenum and tungsten deposits and 2050 ore points relative to each crust and their ratios are identified.