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热液成矿分带是一种输运－反应问题。热液成矿分带基本属于渗滤交代分带性质，它是溶解－沉淀波在可渗透介质中形成和传播的结果。本文应用物理化学流体动力学中的渗滤与溶解－沉淀反应耦合过程理论研究溶解－沉淀波的结构特征，并进一步应用多组分耦合系统动力学中的用于原理揭示其形成的动力学机制，最后提出了一种热流成矿分带理论，对热液成矿分带问题的性质、热液成矿分带的本质和热液成矿分带的结构特征与形成机制提出了新认识。
Hydrothermal mineralization is a transport-reaction problem. The hydrothermal ore-forming belts basically belong to the nature of percolation zonation and are the result of formation and propagation of dissolution-precipitation waves in a permeable medium. In this paper, the structural characteristics of the dissolution-precipitation wave were studied by using the coupled theory of percolation and dissolution-precipitation reaction in the hydrodynamics of physical chemistry. The kinetic mechanism of the formation of the solution was further applied in the dynamics of the multi-component coupled system Finally, a heat flow mineralization zoning theory is put forward, which brings forward a new understanding of the nature of hydrothermal ore-forming zoning, the nature of hydrothermal ore-forming zoning and the structural features and formation mechanism of hydrothermal ore-forming zoning.