本文主要阐述了我国沉积-改造型层控铅锌矿床的地质特征,铅、硫、氢、氧稳定同位素的组成,改造热液的物理化学性质及其来源,Pb、Zn元素的活化迁移和沉淀的实验研究,矿床的成矿规律等。认为矿床的形成首先是成矿物质与含矿岩系同生沉积,又受后期地质作用影响而被改造及进一步富集成矿。整个成矿过程与岩浆活动没有明显联系。 This paper mainly expounds the geological characteristics, the compositions of stable lead, sulfur, hydrogen and oxygen isotopes, the physical and chemical properties of hydrothermal fluids and their origin, the activation and migration of Pb and Zn elements in the sedimentary-remodeling stratabound lead-zinc deposits in China Experimental study, metallogenic regularity of deposits and so on. It is considered that the formation of the deposit is firstly the sedimentation of ore-forming materials and ore-bearing rock series, and is further transformed and further enriched by the influence of later geology. The entire mineralization process and magma activity is not significantly linked.