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宝贝金矿位于新疆西准噶尔地区东南部,与哈图金矿同属于哈图-萨尔托海金成矿带。矿区出露地层为下石炭统太勒古拉组(C1t),岩性主要为中酸性的晶屑凝灰岩和凝灰质粉砂岩;侵入岩主要为似斑状花岗岩岩体。矿区主要发育NNE向断裂和SN向、EW向、NE向和NW向构造裂隙。宝贝金矿似斑状花岗岩岩体和围岩中均有矿化发育。似斑状花岗岩由钾长石、斜长石、石英和少量褐色黑云母组成,斑晶以石英和长石为主,发育绢云母化、角岩化和弱绿泥石化蚀变。岩体显示出很好的Cu、
Baby Gold Mine is located in the southeastern part of West Junggar in Xinjiang, and belongs to the Hatu-Salto Sea gold metallogenic belt with the Hatu gold deposit. The outcropped strata in the mining area are the Lower Carboniferous Tethlechu Formation (C1t). The lithology is mainly of acid-rich crystal tuff and tuffaceous siltstone. The intrusive rocks are mainly plagioclase granite. The mining area mainly develops NNE trending faults and SN trending, EW trending, NE trending and NW tectonic fractures. Baby gold like plagioclase granite and rock are mineralized development. Porphyry-like granites consist of potash feldspar, plagioclase, quartz and a small amount of brown biotite. The phenocrysts are dominated by quartz and feldspar and developed sericitization, hornfaction and weak chlorite alteration. Rock mass shows good Cu,