火山成因矿床中金-银矿化与锡-银矿化的关系

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近年来,在文献中就锡矿化和金矿化的关系问题发表了各种不同的观点。彼特罗夫斯卡娅(1973)认为,锡和钨、钼矿物构成的组合属于金矿床的排斥性的、非典型的矿物组合。涅克拉索夫(1973)以深成矿床为例指出,金和锡不是对抗元素,能形成这两种元素高度富集的综合矿床。马凯耶夫和波利托夫(1972)指出,苏联东部的中生代褶皱带的含锡构造中,锡矿化和金-银矿化在空间上是共生的。 In recent years, various opinions have been published in the literature on the relationship between tin mineralization and gold mineralization. Petrovskaya (1973) argues that the combination of tin and tungsten and molybdenum minerals belongs to the exclusive, atypical mineral assemblage of gold deposits. Necrasov (1973), taking the Shencheng gold deposit as an example, points out that gold and tin are not antagonistic elements and can form a comprehensive deposit with these two elements highly enriched. Mackayev and Pollitov (1972) pointed out that tin mineralization and gold-silver mineralization are spatially symbiotic in the tin-bearing formation of the Mesozoic fold belt in the eastern Soviet Union.
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