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扎西康铅锌锑银矿区主要出露下侏罗统地层。矿区内目前发现的4个铅锌锑银矿体,主要充填于近南北向张扭性断裂破碎带及次级羽状张节理中,矿化强度从构造带中心向两侧围岩呈渐变过渡关系。初步分析矿床与北部的穷多江变质核杂岩、广泛发育的南北向断裂及侏罗纪地层有着密切成因联系。F42、F46、F48所围限的倒三角形区域内的侏罗纪地层、南北向深大断裂和褶皱核部区域,应为今后矿区及外围进一步探矿的重点和主要研究对象。
Zhaxikang Pb-Zn-Sb-Ag ore area mainly exposed Lower Jurassic strata. The four lead-zinc-antimony silver ore bodies currently found in the mining area mainly fill in the near-north-trending tension-torsional fracture zone and the secondary feather-tangential joints. The mineralization intensity gradually changes from the center of the tectonic belt to the surrounding rock relationship. Preliminary analysis of the deposit is closely related to the Qudaojiang metamorphic core complex in the north, the extensive north-south fault and the Jurassic strata. The Jurassic strata, north-south trending faults and fold core areas in the inverted triangle area confined by F42, F46 and F48 should be the focus and main research object for further prospecting in the future mining area and periphery.