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近十余年来,国际上对于磁黄铁矿的研究有大量的文献报道,主要是根据对磁黄铁矿(Fe—S系列)的实验研究,结合热力学及相平衡的基本理论,获得了许多确切资料。这些实验研究都是用已知物料在给定温度、压力及一定时间内完成的。因此有可能将其与天然产出的磁黄铁矿进行对比,以便推导出天然磁黄铁矿所含的Fe原子(％),估算其形成的温度。按与其共生的闪锌矿情况,还可间接地估算它形成时的压力。运用这些数据,结合矿床的地质条件,就有可能为生产及科研提供有意义的资料。
In recent ten years, there are a lot of international reports on pyrrhotite, mainly based on the experimental study of pyrrhotite (Fe-S series) and the basic theory of thermodynamics and phase equilibrium A lot of exact information. These experimental studies are done using known materials at a given temperature, pressure and time. It is therefore possible to compare this with naturally occurring pyrrhotite to derive the Fe atoms (%) contained in the natural pyrrhotite and estimate the temperature at which it is formed. According to the symbiotic sphalerite, it can also indirectly estimate the pressure of its formation. Using these data, combined with the geological conditions of the deposit, it is possible to provide meaningful information for production and research.