成矿作用动力学是地球化学动力学的一个重要分支学科，近年给出了更完善的定义，初步建立了一套理论体系和研究方法。水岩相互作用及动力学模型、物质输运与化学反应、成矿元素的输运与沉淀、化学热力学与输运性质等方面的研究取得许多新的进展。最后指出了成矿作用动力学的某些发展趋势。 Mineralization kinetics is an important branch of geochemical kinetics. In recent years, a more complete definition has been given and a set of theoretical systems and research methods have been initially established. Water-rock interaction and dynamics model, material transport and chemical reactions, transport and deposition of mineral elements, chemical thermodynamics and transport properties and many other aspects of the study made many new advances. Finally, some trends of the metallogenic dynamics are pointed out.