Jollands, MichaelO'Neill, HughHermann, Joerg2015-12-070010-7999http://hdl.handle.net/1885/20039The diffusion, substitution mechanism and solubility limits of Zr and Hf in synthetic forsterite (Mg2SiO4) and San Carlos olivine (Mg0.9Fe0.1)2SiO4 have been investigated between 1,200 and 1,500 °C as a function of the chemical potentials of the componenThe importance of defining chemical potentials, substitution mechanisms and solubility in trace element diffusion studies: the case of Zr and Hf in olivine201410.1007/s00410-014-1055-x2015-12-07