Variation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa

Author:

Woodland A.B,Koch M

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference65 articles.

1. Oxidation status of the mantle: Past and present;Arculus;Annu. Rev. Earth Planet. Sci.,1985

2. J.-P. Poirier, Introduction to the Physics of the Earth’s Interior, Cambridge University Press, Cambridge, 1991, 264 pp.

3. D.H. Eggler, D.R. Baker, Reduced volatiles in the system C-O-H: Implications to mantle melting, fluid formation, and diamond genesis, in: S. Akimoto, M.H. Manghnani (Eds.), High Pressure Research in Geophysics, Centre for Acad. Publ., Tokyo, 1982, pp. 237–250.

4. Fluid phases and the redox state of the Earth’s mantle: Extrapolations based upon experimental, phase-theoretical and petrological data;Woermann;Fortschr. Mineral.,1985

5. Mantle oxidation state and its relationship to tectonic environment and fluid speciation;Wood;Science,1990

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