在含金区的远景评价中,除地质—矿物资料外,关于矿化发育的物理化学条件和主要金共生组合形成参数的最佳组合资料起着重要作用.预测隐伏矿化的重要理论前提是证明热状况特征的稳定保存程度(270—190℃).(HCO_3~-—Cl~-—Ca~(2+)—Mg~(2+)—Na~+)和含金溶液本身的不均匀状态.在不同深度矿床形成过程中,参数差异不大,未发现与成矿省的地质构造和成矿特征有关系。所研究出的含金性温压地球化 In the long-term evaluation of the gold-bearing area, besides the geological-mineral data, the physicochemical conditions for mineralization development play an important role in the optimal combination of the formation parameters of the major gold symbiotic combinations.It is an important theoretical premise for the prediction of concealed mineralization It is proved that the stable storage of thermal characteristics (270-190 ℃) and the heterogeneity of (HCO_3 ~ --Cl ~ - Ca ~ (2 +) - Mg ~ (2 +) - Na ~ +) In the process of deposit formation at different depths, there is not much difference in the parameters, and it is not found to be related to the geological structure and metallogenic characteristics of the metallogenic province. The study of the gold temperature and pressure geochemistry