Diffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1300 degrees C with some geochemical implications

Spandler, CarlO'Neill, Hugh2015-12-100010-7999http://hdl.handle.net/1885/56877Lattice diffusion coefficients have been determined for 19 elements (Li, Be, Na, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Zn, Y, Zr, Eu, Gd, Lu and Hf) in a single crystal of San Carlos olivine as a function of crystallographic orientation, at 1,300°C, 1 bar aKeywords: basalt; crystal chemistry; crystallography; diffusion; geochemistry; lattice dynamics; mantle source; olivine; partition coefficient; trace element Basalt; Crystal chemistry; Diffusion; Mantle; Olivine; Trace elementsDiffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1300 degrees C with some geochemical implications201010.1007/s00410-009-0456-82016-02-24