前言气相色谱法在测定矿物中包裹流质成分组成方面的广泛应用,显示了该方法的优越性。该法使通过对流质挥发物的测量评价可能存在的矿床,尤其是对确定矿脉中矿体的分布成为可能。在矿脉研究中,我们已建立了高度非均匀性的流质系统。这些研究同样强调了形成矿脉的热液系统的非均匀性。由此需要研制一项专门技术,以研究脉石矿物中流体成分分配的规律。 Preface The wide application of gas chromatography in determining the composition of fluid inclusions in minerals shows the superiority of this method. This method makes it possible to evaluate potential deposits by measuring the volatiles of the liquid phase, and in particular to determine the distribution of ore bodies in the veins. In vein research, we have established a highly heterogeneous fluid system. These studies also emphasize the heterogeneity of hydrothermal systems that form veins. This requires the development of a specialized technique to study the law of fluid composition distribution in gangue minerals.