论文部分内容阅读
目前对于地幔岩部分熔融过程中Fe同位素分馏的研究较为广泛,普遍认为熔体富集重Fe同位素,残余地幔富集轻Fe同位素。相对于地幔岩部分熔融过程中Fe同位素分馏的研究,岩浆结晶分异过程中Fe同位素分馏的研究相对较
At present, there is a wide range of research on Fe isotope fractionation in the partial melting of mantle rocks. It is generally believed that the melt is enriched in heavy Fe isotopes and the remaining mantle enriches with light Fe isotopes. Compared with the research of Fe isotope fractionation in the partial melting of mantle rock, the study of Fe isotope fractionation in the process of crystallization differentiation