;
Lead and selenium mainly exist in galena, clausthalite, and selenio-galena which occur as cell-filling of coal-forming plants and are of chemical-sedimentary origin.
铅和
主要赋存在方铅矿、铅矿和方铅矿中，这3种矿
胞腔充填形式出现，属于
学沉积成因。
铅Lead and selenium mainly exist in galena, clausthalite, and selenio-galena which occur as cell-filling of coal-forming plants and are of chemical-sedimentary origin.
铅和主要赋存在方铅矿、铅矿和方铅矿中，这3种矿胞腔充填形式出现，属于学沉积成因。
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