Oxygen fugacity controls in the Earth's upper mantle
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[1] B. Wood,et al. Mantle Oxidation State and Its Relationship to Tectonic Environment and Fluid Speciation , 1990, Science.
[2] A. E. Ringwood,et al. Slab-mantle interactions , 1989 .
[3] B. Wood,et al. The oxidation state of the Earth's sub-oceanic mantle from oxygen thermobarometry of abyssal spinel peridotites , 1989, Nature.
[4] M. Rutter,et al. Upper Mantle Oxygen Fugacity and Its Relationship to Metasomatism , 1989, The Journal of Geology.
[5] W. McDonough,et al. Compositional constraints on the continental lithospheric mantle from trace elements in spinel peridotite xenoliths , 1989, Nature.
[6] D. Green,et al. Mantle metasomatism by ephemeral carbonatite melts , 1988 .
[7] D. Green,et al. Measurement of reduced peridotite-C-O-H solidus and implications for redox melting of the mantle , 1988, Nature.
[8] B. Wood,et al. Magnetite activities across the MgAl2O4-Fe3O4 spinel join, with application to thermobarometric estimates of upper mantle oxygen fugacity , 1988 .
[9] H. O’Neill,et al. The Olivine—Orthopyroxene—Spinel Oxygen Geobarometer, the Nickel Precipitation Curve, and the Oxygen Fugacity of the Earth's Upper Mantle , 1987 .
[10] H. O’Neill. Quartz-fayalite-iron and quartz-fayalite-magnetite equilibria and the free energy of formation of fayalite (Fe 2 SiO 4 ) and magnetite (Fe 3 O 4 ) , 1987 .
[11] C. Langmuir,et al. Oxidation states of mid-ocean ridge basalt glasses , 1986 .
[12] B. Murck,et al. The effects of temperature, oxygen fugacity and melt composition on the behaviour of chromium in basic and ultrabasic melts , 1986 .
[13] S. Haggerty. Diamond genesis in a multiply-constrained model , 1986, Nature.
[14] E. Mathez. Influence of degassing on oxidation states of basaltic magmas , 1984, Nature.
[15] S. H. Richardson,et al. Origin of diamonds in old enriched mantle , 1984, Nature.
[16] M. Rivers,et al. The ferric-ferrous ratio of natural silicate liquids equilibrated in air , 1983 .
[17] S. Haggerty,et al. Redox state of Earth's upper mantle from kimberlitic ilmenites , 1983, Nature.
[18] D. Eggler. Upper mantle oxidation state: Evidence from olivine‐orthopyroxene‐ilmenite assemblages , 1983 .
[19] A. E. Ringwood,et al. Phase Transformations and Differentiation in Subducted Lithosphere: Implications for Mantle Dynamics, Basalt Petrogenesis, and Crustal Evolution , 1982, The Journal of Geology.
[20] M. Fisk,et al. Experimental crystallization of chrome spinel in FAMOUS basalt 527-1-1 , 1980 .
[21] Robert W. Nesbitt,et al. Geochemical characteristics of mid-ocean ridge basalts , 1979 .
[22] Motoaki Sato,et al. Oxygen fugacity of basaltic magmas and the role of gas-forming elements , 1978 .
[23] B. Wood,et al. Ferric iron in mantle-derived garnets , 1990 .
[24] R. Arculus. Oxidation Status of the Mantle: Past and Present , 1985 .
[25] J. Dawson,et al. Oxidation states of the upper mantle recorded by megacryst ilmenite in kimberlite and type A and B spinel lherzolites , 1984 .
[26] D. Baker,et al. Reduced Volatiles in the System C-O-H: Implications to Mantle Melting, Fluid Formation, and Diamond Genesis , 1982 .
[27] 日本学術振興会,et al. High-Pressure Research in Geophysics , 1982 .