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采用地质类比方法， 结合秦岭造山带热水沉积岩相研究， 提出热水沉积体系概念。通过现代陆相及海相热泉和秦岭热水沉积岩相对比， 按化学成分可将古热水场划分为强酸性硫酸盐型、弱酸强碱碳酸盐型、以ＳｉＯ２ 为酸酐型、碱性富Ｍｇ 重卤水型、热卤水型及强酸性硼硅酸盐型等６ 种类型古热水场。并对典型热水场的地球化学类型特征及成岩成矿作用进行了讨论。在前人研究的基础上， 探讨了热水系统的流体地球化学动力学。提出了热水沉积成矿盆地中热水系统的两类地球化学流体动力学模型， 热水层流体系模型和不同成分、性状的热水混合体系模型。从热水系统的边界协同学约束条件、空间拓朴结构、流体通量动量方程及矿质大规模沉淀的地球化学动力学等方面对这两类流体动力学模型进行了讨论。
Geological analogy, combined with hydrothermal sedimentary facies research Qinling orogenic zone, put forward the concept of hot water deposition system. Through the comparison of the modern terrestrial and marine hot springs with the Qinling hot-water sedimentary rocks, the pale-hot water field can be divided into strong acid sulfate and weak acid strong alkali carbonate according to the chemical composition, SiO2 as the anhydride type, alkaline Mg-rich heavy brine type, hot brine type and strong acid borosilicate type 6 types of ancient hot water. The geochemical characteristics and diagenesis and mineralization of typical hydrothermal reservoirs are also discussed. Based on the previous studies, the fluid geochemistry of hot water system is discussed. Two types of geochemical hydrodynamics model, hot water laminar flow system model and hot water mixed system model with different composition and traits are proposed. These two kinds of fluid dynamics models are discussed from the aspects of boundary synergetic constraints, spatial topological structure, fluid flux momentum equation and geochemical kinetics of mass mineralization of hot water system.