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据磁铁矿研究资料评价岩浆杂岩体成因和相关性上述各篇资料指出,不论那个成因族的磁铁矿它的一套特征模式主要受原始熔融体(溶液)的地球化学特征和结晶过程温度的影响。无疑地 Eh=Ph 和挥发条件这些热动力学的参数在某种情况下起重大作用,不过、在大多数情况下,这影响统一于干两个主要的因素,固相上的压力影响是可以忽视的,这是因为所研究的全部磁铁矿都属于不深的(0-12km)部位的缘故。附表1是由各种成分岩浆岩获得的磁铁矿平均成分,引用的这些结果由作者提供的之外,还有早期资料所引用的造岩元素(Ti、Mn、Mg、Al)资料,以及所引用的分析结果,文献出外。
Magnetite research data to evaluate the genesis and correlation of magmatic complexes The above data indicate that the set of characteristic modes of magnetite regardless of that gene family is mainly affected by the geochemical characteristics of the original melt (solution) and the crystallization process Effect of temperature. Undoubtedly Eh = Ph and the volatilization conditions These thermodynamic parameters play a significant role in some cases, however, in most cases this affects the two main factors that are uniformed in the dry. The pressure effect on the solid phase can be Ignored, this is because all the magnetite studied belongs to the less deep (0-12km) part of the reason. Schedule 1 is the average composition of magnetite obtained from various constituents of magmatic rocks. These results are provided by the authors as well as from the rock-forming elements (Ti, Mn, Mg, Al) cited in earlier sources, As well as the analysis results quoted, the literature is out.