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已有的地质、地球物理和地球化学证据表明太古宙Ａｕ－石英脉、低温热液Ａｕ－Ａｇ和Ａｕ矽卡岩成矿流体的主要组分源自岩浆，而且Ａｕ、Ａｇ及有关的富美元素也源自岩浆。太古宙Ａｕ－石英脉、太古宙Ｈｅｍｌｏ型、低温热液Ａｕ－Ａｇ和Ａｕ矽卡岩体系的元素的产出具有重要的共性，表明其具有共同的成因过程。例如，２７个元素中，４４％（ｎ＝１２）的元素出现在１０个矿床亚类的至少７个亚类之中：Ａｕ、Ａｇ、Ｆｅ、Ｃｕ、Ｐｂ、Ｚｎ、Ｈｇ、Ｍｏ、Ｓｂ、Ａｓ、Ｔｅ和ｓ（９个金属、２个类金属和１个非金属）。加上Ｂ和Ｗ，５２％（ｎ＝１４）出现在至少５个亚类之中。富集的亲铜／亲铁元素的出现频率很高，达８５％（２７个元素中的２３个）。总体元素（ｎ＝３１）的出现频率也较高，达７４％（ｎ＝２３）。所有这些主要的亲铜／亲铁元素均富集于太古宙Ａｕ－石英脉、太古宙Ｈｅｍｌｏ型、低温热液Ａｕ－Ａｇ和Ａｕ矽卡岩矿床之中。如果岩浆挥发分的饱和出现在岩浆硫化物熔体／上悬固体因重力而亏损之后，那么Ａｕ、Ａｇ和相关亲铜元素将由于高的硫化物熔体／硅酸盐岩浆的分配系数（１０￣２～１０￣４，如Ａｕ为３ｘ１０￣４，Ｓｅ为１０￣３）而从岩浆中分离出来。因此可以得出，太古宙Ａｕ－石?
The available geological, geophysical and geochemical evidence suggests that the major components of the Archean Au- quartz veins, low-temperature hydrothermal Au-Ag and Au skarn mineralization fluids originate from magma and that Au, Ag and related Euphrates From magma. Archaeozoic Au-quartz veins, Archean Hemlo-type, low-temperature hydrothermal Au-Ag and Au skarn system elements have important commonalities, indicating that they have a common genetic process. For example, of the 27 elements, 44% (n = 12) of the elements appear in at least seven sub-categories of the 10 deposit sub-categories: Au, Ag, Fe, Cu, Pb, Zn, Hg, Mo, Sb, As, Te and s (9 metals, 2 metals and 1 nonmetal). With B and W, 52% (n = 14) appeared in at least 5 subcategories. Enriched pro-copper / pro-iron elements occur at a high rate of 85% (23 of 27 elements). The overall element (n = 31) also appeared at a high frequency of 74% (n = 23). All of these major copper / iron elements are enriched in Archean Au-quartz veins, Archean Hemlo-type, low-temperature hydrothermal Au-Ag and Au skarn deposits. If the saturation of the magma volatiles occurs after the magma sulfide melt / overhang is depleted due to gravity, the Au, Ag and related cupper elements will be depleted due to the high sulphide melt / silicate magma partition coefficient (10 ~ 2 ~ 10 ~ 4, such as Au is 3 × 10 ~ 4, Se is 10 ~ 3) and separated from the magma. It can therefore be concluded that Archean Au-Stones