Experimental Determination of the Temperature Dependence of Ni, Sc, Y, La, Sm and Lu Partition Coefficients Between Pyroxene and Differentiated Mafic Liquids

这项工作将通过实验确定分配行为 Sc、Y、La、Sm、Lu和Ni之间的正辉石和斜辉石， 一系列天然镁铁质硅酸盐岩浆 以前的调查 一直在合成，而不是自然，融化和更高 温度 获得的信息将有助于我们解释 自然岩浆系统在上升过程中的演化方式 在地球内部。

This work will determine experimentally the partitioning behavior of Sc, Y, La, Sm, Lu, and Ni between ortho- and clino pyroxene and a range of natural mafic silicate magmas. Previous investigations have been on synthetic, rather than natural, melts and at higher temperature. The information obtained will help us to interpret the way that natural magmatic systems have evolved as they rose within the earth.