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萨吾斯铅锌矿床位于西伯利亚板块南缘阿尔泰晚古生代活动陆缘的泥盆纪—石炭纪弧后盆地中。矿床赋存于下泥盆统康布铁堡组酸性火山熔岩、火山碎屑岩夹陆源碎屑岩及碳酸盐岩中,是与海相火山作用有关的铅锌矿床。矿区位于1∶5万水系沉积物测量圈定的Pb-Ag-As-Zn-Bi-Cu-Mo-Au-Sb-Co-Ni综合异常内,其中Ag、As、Pb、Zn异常套合较好,与矿体基本对应,特别是Zn异常中心与矿体位置完全对应。矿区激电异常具有低阻、高幅频率、多峰值的特征,与地表矿化蚀变带对应。磁异常与激电异常相对应,异常宽度小于激电异常。TEM测深工作在矿区圈定了3个TEM低阻异常,均处于Ⅱ号矿化蚀变带内。在综合分析矿床成矿地质条件、地球化学异常、地球物理异常特征的基础上,建立了该矿床地质-地球物理-地球化学找矿模式,对类似矿床的发现和评价能够起到借鉴作用。
The Safus Pb-Zn deposit is located in the Devonian-Carboniferous back-arc basin of the Late Paleozoic active margin of the Altay on the southern margin of the Siberian plate. The ore deposits occur in the Lower Devonian Kangbudiebao acidic volcanic lava, pyroclastic clastics, terrigenous clastic rocks and carbonate rocks, and are lead-zinc deposits related to marine volcanism. The mine is located in the comprehensive Pb-Ag-As-Zn-Bi-Cu-Mo-Au-Sb-Co-Ni anomaly delineated by 1:50 000 sediment measurements, , Corresponding to the basic ore body, especially the Zn anomaly center completely corresponded with the ore body position. The characteristics of low-resistivity, high-amplitude frequency and multi-peak of the anomalies in the mine area correspond to the surface mineralized alteration zones. Magnetic anomaly corresponds to an anomalous anomaly, and an anomalous width is less than an anomalous anomaly. TEM sounding work in the mining area delineated three TEM low resistance anomalies, are in Ⅱ mineralized alteration zone. Based on the comprehensive analysis of mineralization geological conditions, geochemical anomalies and geophysical anomalies, the geologic-geophysical-geochemical prospecting model of this deposit is established, which can serve as reference for the discovery and evaluation of similar deposits.