The salt-forming regions for the complex salt−water system in the nonequilibrium state are more complex and do not always follow the solubility diagram. To understand the behaviors of the saltforming region departing from the equilibrium phase area, the experimental investigation of the salt-forming regions in a nonequilibrium state for the quaternary system of Na + , Mg 2+ //Cl − , SO 4 2− −H 2 O at the isothermal boiling temperature of 373 ± 0.2 K was carried out. The 32 specifically saturated solutions were evaporated with an average evaporation intensity of (1.8 to 2.4) g/(L•min)(water). Based on the liquid phase routes and solid precipitated sequence, the solid-forming regions for mainly salts were determined, respectively, where the regions of halite, thenardite, vanthoffite, and loeweite are enlarged, and they are 1.87, 1.76, 1.85, and 1.25 times bigger, respectively, than those solubility region, whereas d'ansite and kieserite regions are reduced. Furthermore the so-called salt-forming diagram composed of the saltforming regions shows the stability of salt-forming regions in the nonequilibrium state, and the so-called isothermal diagram combined a salt-forming diagram with the solubility diagram, giving five one-salt stable regions and a complex conditional region (including eight two-salt regions and four three-salt regions). The conditional region does not exist in the solubility diagram and metastable diagram but exists in the salt-forming diagram and occupies a field about 47 % of the diagram's total area where the salt precipitating depends on nonthermodynamic conditions, such as crystal seed, evaporation intensity, mechanical effects, and so forth. Thus, knowledge of the salt-forming region, especially the conditional salt-forming region, would be extremely valuable to industry process design and control.