Kesson, SusanFitz Gerald, JohnO'Neill, HughShelley, Michael2015-12-130031-9201http://hdl.handle.net/1885/72623The disproportionation products of olivine Fo90 in diamond-anvil cell experiments at about 1 Mbar are magnesian silicate perovskite Mg# ~94 and a series of magnesiowüstites Mg# 85-90, yielding a recommended value of 0.4 ± 0.1 for the distribution coeffiKeywords: iron; magnesiowustite; P-T conditions; partitioning; perovskite; phase transition Magnesian silicate perovskite; Magnesiowüstite; Partioning of ironPartitioning of iron between magnesian silicate perovskite and magnesiowustite at about 1 Mbar200210.1016/S0031-9201(02)00063-82015-12-11