On the nonstoichiometry and point defects of olivine
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Birle JD, Gibbs GV, Moore PB, Smith JV (1968) Crystal structures of natural olivines. Am Mineral 53:807?824
Bershov LV, Gaite JM, Hafner SS, Rager H (1983) EPR-and Endor study of Cr3+-Al3+ pairs in forsterite. Phys Chem Minerals 9:95?102
Cirilli V (1946) Studio dell' equilibrio di riduzione con ossido di carbonio, degli ossidi di ferro in presenza di silice. Gazz Chim Ital 76:331?338
Darken LS (1948) Melting points of iron oxides on silica; Phase equilibria in the system Fe-Si-O as a function of gas composition and temperature. J Am Chem Soc 70:2046?2053
Dieckmann R (1982) Defects and cation diffusion in magnetite (IV): Nonstoichiometry and point defect structure of magnetite (Fe3??O4): Ber. Bunsenges. Phys Chem 86:112?118
Dieckmann R, Schmalzried H (1975) Point defects in oxide solid solutions (III): Mobilities of cations and vacancies in (Co, Ni)O- and (Co, Mg)O-solid solutions and the calculation of correlation factors. Ber. Bunsenges. Phys Chem 79:1108?1119
Duba A, Heard HC, Schock RN (1974) Electrical conductivity of olivine at high pressure and under controlled oxygen fugacity. J Geophys Res 79:1667?1673
Giddings RA, Gordon RS (1973) Review of oxygen activities and phase boundaries in wüstite as determined by EMF and gravimetric Method. J Amer Ceram Soc 56:111?116
Greskovich C, Schmalzried H (1970) Nonstoichiometry and electronic defects in Co2SiO4 and in CoAl2O4-MgAl2O4 crystalline solutions. J Phys Chem Solids 31:639?646
Kitayama K, Katsura T (1968) Composition of fayalite and its standard free energy of formation. Bull Chem Soc Jp 41:525?528
Kitayama K, Katsura T (1968) Activity measurements in orthosilicate and metasilicate solid solutions I. Mg2SiO4-Fe2SiO4 and MgSiO3-FeSiO3 at 1,204° C. Bull Chem Soc Jp 41:1146?1151
Morin FJ, Oliver JR, Housley RM (1977 and 1979) Electrical properties of forsterite Mg2SiO4. Phys Rev (I) B16:1434?1445 (II) B19:2886?2894
Nafziger RH, Muan A (1967) Equilibrium phase compositions and thermodynamic properties of olivines and pyroxenes the system MgO-FeO-SiO2. J Amer Mineral 52:1364?1385
Niebuhr H (1976) Elektron-Spin-Resonanz von dreiwertigem Eisen in Forsterit. Habilitationsschrift, FB Geowissenschaften, Marburg (1976)
Pluschkell W, Ph D-thesis TU Clausthal (1967)
Poumellec M (1979) Autodiffusion du Silicium 30 dans la Forsterite Mg2SiO4. Thesis Orsay
Rizzo HF, Gordon RS, Cutler IB (1969) Determination of phase boundaries and thermodynamic functions in the iron-oxygen system by EMF measurements. J Electrochem Soc 116:266?274
Schmalzried H (1965) Point defects in ternary ionic crystals. In: Progress in Solid State Chemistry 8:265?308
Schmalzried H, Navrotsky A (1975) Festkörperthermodynamik Verlag Chemie, Weinheim, pp. 242?249
Schwab RG, Küstner D (1981) Die Gleichgewichtsfugazitäten technologisch und petrologisch wichtiger Sauerstoffpuffer Neues Jahrb Mineral Abh 140:111?142
Schwab RG, Söhnlein G (1977) Homogene und heterogene Redoxgleichgewichte des Fayalits: Neues Jahrb Mineral Abh 129:15?32
Schwerdtfeger K, Muan A (1966) Activities in olivine and pyroxenoid solid solutions of the system Fe-Mn-Si-O at 1,150° C. Trans Metall Soc AIME 236:201?211
Schwier VG, Dieckmann R, Schmalzried H (1973) Punktfehlstellen in Oxidmischphasen (I) Fehlstellenenthermodynamik der Mischphasen (CoxMg1?x)O und (CoxMgt?x)2 · SiO4. Ber Bunsenges Phys Chem 77:402?408
Sockel HG (1974) Defect structure and electrical conductivity of crystalline ferrous silicate. In: Defects and transport in oxides. Seltzer MS and Jaffe RI (eds). Plenum Press, New York, pp 341?354
Taylor RW, Schmalzried H (1964) The free energy of formation of some titanates, silicates and Mg-aluminate from measurements made with galvanic cells involving solid electrolytes. J Phys Chem 68:2444?2449
Wagner C (1971) The determination of small deviations from the ideal stoichiometric composition of ionic crystals and other binary compounds. In: Progress in Solid State Chem 6:1?14
Weertman J, Weertman JR (1975) High temperature creep of rock and mantle viscosity. In: Annual reviews of earth and planetary sciences, Donath FA, Stehli FG and Wetherill GW (eds). Vol 3, pp 293?315
Williams RJ (1971) Reaction constants in the system Fe-MgO-SiO2-O2 at 1 bar between 900° C and 1,300° C: Experimental results: Am J Sci 271:132?146
Wones DR, Gilbert MC (1969) The fayalite-magnetite-quartz assemblage between 600° C and 800° C. Am J Sci 267:480?488