Berry, Andrew JohnO'Neill, HughHermann, JoergScott, Dean2015-12-080012-821Xhttp://hdl.handle.net/1885/33585Forsterite crystals were synthesised under water saturated conditions at 1400 °C and 1.5 GPa doped with trace amounts of either B, Al, Sc, Ti, V, Cr, Mn, Fe, Co, Ga, Y, Zr, In, Sm, Gd, Dy, Tm, or Lu. The common and intense hydroxyl stretching bands inKeywords: Forsterite; Nominally anhydrous minerals; Experimental mineralogy; Infrared spectroscopy; Petrology; Substitution reactions; Synthesis (chemical); Trace elements; Olivine; experimental mineralogy; forsterite; infrared spectroscopy; olivine; trace element experimental petrology; hydrated defects; infrared spectroscopy; mantle water; nominally anhydrous minerals; olivine; trivalent trace elements200710.1016/j.epsl.2007.06.0212015-12-08