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金-锑和金-银建造的矿床在世界许多矿区广为发育,但它们在空间上到处都是没有联系的。在太平洋矿带中,金-银矿床分布在外带,而金-锑矿床则分布在内带。在这些地带的接触部位有时形成过渡的金-锑-银建造矿床。在上述矿床中金和锑是以不同数量关系参与的普遍的元素。至于银,则对金-锑建造矿床来说这一元素并不是典型的。并且极少以杂质的形式遇到。 金-银建造和金-锑建造矿床的矿石在地球化学属性方面的明显差别是由它们形成时所处的地质环境、金属来源以及物理-化学参数等的特性所造成的。首先我们发现,所
Gold-antimony and gold-silver deposits are widely developed in many mining areas around the world, but they are spatially unconnected. In the Pacific ore belt, the gold-silver deposits are located in the outer belt, while the gold-antimony deposits are located in the belt. Transitional gold-antimony-silver deposits are sometimes formed at the contact sites in these areas. Gold and antimony are common elements involved in different quantities in these deposits. As for silver, this element is not typical for gold-antimony ore deposits. And rarely encountered in the form of impurities. Significant differences in geochemical properties of gold-silver-built and gold-antimony ore deposits result from the geological environment, metal sources, and physico-chemical properties of the minerals in which they were formed. First of all, we found that