中文摘要:底苏铅锌矿床是近年米发现的。该矿床具“双源”沉积改造特征。同生沉积成岩成矿阶段同时存在海底热水和正常海水沉积作用，形成热水沉积矿石及矿源层。大气降水热液改造成矿阶段，大气降水沿岩石裂隙下渗被加热并淋滤早期沉积矿石及矿源层中的Pb、Zn，使之以[PbCl20]、[ZnCl20]迁移，当含矿热液运移拿有利构造部位时，Pb、Zn络合物交代地层中的黄铁矿或被有机质还原向再沉淀成矿。本文在矿床地球化学研究基础上，提出了底苏铅锌矿脒的成矿模式。
Abstract:The Disu ore deposit , one of the lead-zinc deposits discovered in recent years, is characterized by "double source" sedimentary transformation. In the syndepositional diagenetic and ore-forming stage there existed both submarine hot water deposition and normal seawater deposition, forming the hot water sedimentary ore and the source bed, During the meteoric water and hydrothermal transformation ore-forming stage, the downward percolating meteoric water along fissures was heated and then leached lead and zinc from the early-deposited ore and source bed, resulting in the migration of these elements in the form of [PbCl20] and [ZnCl20].When ore-bearing hydrothermal solution moved to the favorable structural and lithologic position, Pb-Zn complexes replaced pyrite in strata or were reduced by organic matter, and eventually formed the ore deposit through reprecipitation. Based on geochemical studies, the present paper puts forward a metallogenic model for the Disu lead-zinc deposit.
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基金项目:四川地矿局八五科研项目（85-01-1）
引用文本：
朱赖民, 栾世伟, 袁海华, 戚华文.1998.论底苏铅锌矿床的“双源”沉积改造成矿模式[J].矿床地质,17(1):82~90.1998.“Double source” sedimentary-transforation metallogenic model of the disu lead-zinc deposit[J].Mineral Deposits17(1):82~90
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