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通过对底舒铅锌矿床地层岩石和矿石稀土元素地球化学研究，作者认为，同生沉积成岩成矿阶段矿层（或矿源层）中的金属组分主要来自海底合矿热水和正常海水沉积物，热液改造阶段矿石中的金属组分源自沉积成岩成矿阶段矿层和矿区外围地层。
Based on the REE geochemistry of the strata and rocks in the Shuzu lead-zinc deposit, the authors believe that the metal components in the ore-bearing strata (diagenetic and mineralogical stages) of the sedimentary diagenesis are mainly derived from the seabed ore-forming hot water and normal seawater sediments The metal components in the ores during the hydrothermal reforming stage originated from sedimentary diagenetic and ore-forming stages and outlying formations.