流体以成矿溶液和搬运介质的形式参与各种成矿作用。在20世纪50—60年代,流体-岩石实验主要与成矿作用或地热体系研究有关,研究的重点主要集中在:反应过程中溶液化学变化、反应岩石的蚀变和新相的形成、岩石物理化学性和溶液化学的关系等(曾贻善,2003)。1970年,国际地球化学和宇宙化学协会(IAGC)设水-岩相 Fluid is involved in various mineralization in the form of ore-forming solutions and transport media. In the 1950s and 1960s, fluid-rock experiments were mainly related to metallogenesis and geothermal systems. The research focuses mainly on the chemical reactions of solution, the alteration of reaction rocks and the formation of new facies, the petrophysics Chemical and solution chemistry (Zeng Yi, 2003). In 1970, the IAGC set up water-facies