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所研究矿床为火山带金-银建造的典型代表。它们产于晚白垩世火山岩(英安岩、安山岩)中,构成以钾强烈带出为特点的巨厚交代蚀变岩带。这些蚀变岩带内部被含冰长石的石
The deposit studied is a typical representative of volcanic gold-silver construction. They are produced in the Late Cretaceous volcanic rocks (dacite, andesite), constituting a metamorphosed metamorphic rock zone that is characterized by the strong uptake of potassium. Within these altered rocks are feldspar-bearing rocks