Influence of protons on Fe‐Mg interdiffusion in olivine

By S. Hier‐Majumder, I. Anderson, D. Kohlstedt. 2004

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Fe–Mg diffusion in olivine II: point defect chemistry, change of diffusion mechanisms and a model for calculation of diffusion coefficients in natural olivine (2007, background): “Notwithstanding the experimental challenge in carrying out the measurements reported in NS83 and TD02, the data do not completely represent the situation for natural olivines that always contain a variety of trace elements (e.g., Ni, Mn, Cr, Al, Ti, H, P). Other than for the rather specialized case ”
Fe–Mg diffusion in olivine I: experimental determination between 700 and 1,200°C as a function of composition, crystal orientation and oxygen fugacity (2007, background): “Buening and Buseck 1973; Misener 1974; Morioka 1981; Nakamura and Schmalzried 1984; Jurewicz and Watson 1988; Morioka and Nagasawa 1991; Chakraborty et al. 1994; Chakraborty 1997; Jaoul et al. 1995; Ito et al. 1999; Petry et al. 2004; Coogan et al. 2005; Hier-Majumder et al. 2005 ).”