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Woodland, A.B, Koch, M (2003) Variation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa. Earth and Planetary Science Letters, 214 (1) 295-310 doi:10.1016/s0012-821x(03)00379-0

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Reference TypeJournal (article/letter/editorial)
TitleVariation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa
JournalEarth and Planetary Science Letters
AuthorsWoodland, A.BAuthor
Koch, MAuthor
Year2003 (September)Volume214
Page(s)295-310Issue1
PublisherElsevier BV
DOIdoi:10.1016/s0012-821x(03)00379-0Search in ResearchGate
Mindat Ref. ID377265Long-form Identifiermindat:1:5:377265:6
GUIDc1772a9d-219a-4661-8477-6f2a6b02ef26
Full ReferenceWoodland, A.B, Koch, M (2003) Variation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa. Earth and Planetary Science Letters, 214 (1) 295-310 doi:10.1016/s0012-821x(03)00379-0
Plain TextWoodland, A.B, Koch, M (2003) Variation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa. Earth and Planetary Science Letters, 214 (1) 295-310 doi:10.1016/s0012-821x(03)00379-0
In(2003, September) Earth and Planetary Science Letters Vol. 214 (1) Elsevier BV

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

J.-P. Poirier, Introduction to the Physics of the Earth’s Interior, Cambridge University Press, Cambridge, 1991, 264 pp.
Woermann (1985) Fortschr. Mineral. Fluid phases and the redox state of the Earth’s mantle: Extrapolations based upon experimental, phase-theoretical and petrological data 63, 263
Wood (1991) Rev. Mineral. Oxygen barometry of spinel peridotites 25, 417
S. Haggerty, Redox state of the continental lithosphere, in: M. Menzies (Ed.), Continental Mantle, Oxford Monogr. Geol. Geophys. 16, Oxford Univ. Press, Oxford, 1990, pp. 87–109.
K.G. Cox, J.J. Gurney, B. Harte, Xenoliths from the Matsoku pipe, in: P.H. Nixon (Ed.), Lesotho Kimberlites, Lesotho National Development Corp., Meseru, 1973, pp. 76–91.
F.R. Boyd, High- and low-temperature garnet peridotite xenoliths and their possible relation to the lithosphere-asthenosphere boundary beneath southern Africa, in: P.H. Nixon (Ed.), Mantle Xenoliths, Wiley, Chichester, 1987, pp. 403–412.
Woodland (2002) Eur. J. Mineral. Beih. (abs) Clinopyroxene as an indicator of mantle processes; Heterogeneities at the millimetre scale in South African peridotite xenoliths 14, 179
Amthauer (1976) Z. Kristallogr. The Mössbauer spectrum of 57Fe in silicate garnets 143, 14
F.R. Boyd, D.G. Pearson, S.A. Mertzman, Spinel-facies peridotites from the Kaapvaal root, in: J.B. Dawson (Ed.), Proc. 7th Kimberlite Conf., Redroof Publ., Cape Town, 1999, pp. 40–48.
Not Yet Imported: High‐Pressure Research in Mineral Physics: A Volume in Honor of Syun‐iti Akimoto - book-chapter : 10.1029/GM039p0231

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A.B. Woodland, P. Peltonen, Ferric iron contents of garnet and clinopyroxene and estimated oxygen fugacities of peridotite xenoliths from the Eastern Finland Kimberlite Province, in: P.H. Nixon (Ed.), Proc. 7th Kimberlite Conference, Redroof Publishers, Cape Town, 1999, pp. 904–911.
D. Smith, Temperatures and pressures of mineral equilibration in peridotite xenoliths: Review, discussion, implications, in: Y. Fei, C.M. Bertka, B.O. Mysen (Eds.), Mantle Petrology: Field Observations and High Pressure Experimentation: A tribute to Francis R. (Joe) Boyd, Geochem. Soc. Spec. Publ. 6, 1999, pp. 171–188.
Woodland (1993) Am. Mineral. Synthesis and stability of Fe32+Fe23+Si3O12 garnet and phase relations with Fe3Al2Si3O12-Fe32+Fe23+Si3O12 solutions 78, 1000
Not Yet Imported: Evolution of the Earth and Planets - book-chapter : 10.1029/GM074p0073

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Woodland (1996) J. Conf. Abstr. The ferric iron budget of orogenic lherzolite massifs and implications for the mantle redox state 1, 687
Wallace (1994) Am. Mineral. S speciation in submarine basaltic glasses as determined by measurements of Skα X-ray wavelength shifts 79, 161


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