Kamechatka表生金矿床位于中新世—第四纪火山机构的中心。主岩为基性、中性和酸性成分的火山碎屑岩和喷出岩,它们已被由玄武岩、安山岩、英安岩和闪长岩等各种脉岩和岩体所穿切。通过近期火山活动和许多热泉的存在而证买了矿区的现代活动。 矿体呈脉状、细脉状,一般为南北走向。根据矿石组分可以划分出2种矿石类型:硫化物-多金属,含金;低硫化物,金石-英-碳酸盐。矿石矿物成分变化很大,天然矿物有自然金和自然银,磁化物有 The Kamechatka epigenetic gold deposit is located in the center of the Miocene-Quaternary volcano. The host rock is a volcaniclastic and extrusive rock that is a basic, neutral and acidic component that has been cut by various vein and rock masses such as basalts, andesite, dacite and diorite. The modern activities of the mines have been purchased through the recent volcanic activity and the presence of many hot springs. Ore body is veins, veins, generally north-south direction. According to the ore components can be divided into two types of ore: sulfide - polymetallic, gold; low sulfide, gold stone - British - carbonate. Ore minerals vary greatly in composition, natural minerals have natural gold and natural silver, there are magnetizers