Solid Solution Models and Data
Part of the Data and Knowledge in a Changing World book series (DATAKNOWL)
An ionic model with mixing occurring in the first sublattice is applied to olivine, 13- and y-spinel phases, described by the formula (Fe+2,Mg+2)2(Si+4)(0-2)4. The end-members are Fe2SiO4 and Mg2SiO4.
KeywordsEnthalpy Geochemistry Olivine Perovskite Dine
Unable to display preview. Download preview PDF.
© Springer-Verlag Berlin Heidelberg 2004