金—锑和金—银建造矿床在世界的很多矿化地区广泛发育,但它们在空间上普遍地被分开.在太平洋矿化带,金—银矿床位于外带,而金—锑矿床位于内带.在这个带连接的地区,有时形成过渡的金—锑—银建造的矿床.上述矿床中,金和锑在不同的数量关系中是主要的.至于谈及银,对金—锑建造矿床来说,这种元素不典型和极少看到化合物形式. Gold-antimony and gold-silver deposits are widely developed in many mineralized areas of the world, but they are generally spatially separated. In the Pacific mineralization belt, the gold-silver deposit is located in the outer zone and the gold-antimony deposit is located in the In this connected area, transitional gold-antimony-silver deposits are sometimes formed, of which gold and antimony are dominant in different quantitative relationships. As for silver, the deposit of gold-antimony For the most part, this element is not typical and rarely seen as a compound.