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胜利沟-红灯沟金矿床处于南祁连岛弧带西段的团鱼山—滩间山岛弧带反“S”型构造西侧的加里东、华力西期金、铅、锌成矿带(区)之赛什腾山—布赫特山金、铅、锌、铜成矿带上,具有较好的成矿地质条件。矿区地层为一套浅变质的火山-沉积岩系,包括安山熔岩、安山质火山碎屑凝灰岩、凝灰质砂砾岩、含钙质凝灰岩、石灰岩等。火山活动强烈,发育很厚的火山熔岩-火山碎屑岩-火山沉积岩,
The Shengligou-Hongdengou gold deposit is located in the Galliferous and Hurricane West gold belt of the anti-S-shaped structure at Tuanyuashan-Tanjianshan Island arc belt in the western section of the arc belt of South Qilian Island. Zinc metallogenic belt (area) of the Saishiteng - Buhu Te mountains gold, lead, zinc, copper metallogenic belt, with good geological conditions of mineralization. The mine strata are a set of metamorphic volcanic-sedimentary rocks, including andesitic lava, andesitic volcaniclastic tuff, tuffaceous conglomerate, calcareous tuff, and limestone. Volcanic activity, the development of thick volcanic lava - pyroclastic rocks - volcanic sedimentary rocks,