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References

  • Asimow, P. D., and M. S. Ghiorso (1998), Algorithmic modifications extending MELTS to calculate subsolidus phase relations, Am. Mineral., 83(9–10), 11271132.
  • Asimow, P. D., and C. H. Langmuir (2003), The importance of water to oceanic mantle melting regimes, Nature, 421(6925), 815820.
  • Asimow, P. D., and E. M. Stolper (1999), Steady-state mantle-melt interactions in one dimension: I. Equilibrium transport and melt focusing, J. Petrol., 40(3), 475494.
  • Asimow, P. D., M. M. Hirschmann, and E. M. Stolper (2001), Calculation of peridotite partial melting from thermodynamic models of minerals and melts, IV. Adiabatic decompression and the composition and mean properties of mid-ocean ridge basalts, J. Petrol., 42(5), 963998.
  • Asimow, P. D., J. E. Dixon, and C. H. Langmuir (2004), A hydrous melting and fractionation model for mid-ocean ridge basalts: Application to the Mid-Atlantic Ridge near the Azores, Geochem. Geophys. Geosyst., 5, Q01E16, doi:10.1029/2003GC000568.
  • Bacon, C. R., and T. H. Druitt (1988), Compositional evolution of the zoned calcalkaline magma chamber of Mount Mazama, Crater Lake, Oregon, Contrib. Mineral. Petrol., 98(2), 224256.
  • Baker, M. B., and E. M. Stolper (1994), Determining the composition of high-pressure mantle melts using diamond aggregates, Geochim. Cosmochim. Acta, 58(13), 28112827.
  • Berman, R. G., and A. M. Koziol (1991), Ternary excess properties of grossular-pyrope-almandine garnet and their influence in geothermobarometry, Am. Mineral., 76(7–8), 12231231.
  • Blundy, J., and B. Wood (1994), Prediction of crystal-melt partition coefficients from elastic moduli, Nature, 372(6505), 452454.
  • Blundy, J. D., T. J. Falloon, B. J. Wood, and J. A. Dalton (1995), Sodium partitioning between clinopyroxene and silicate melts, J. Geophys. Res., 100(B8), 15,50115,515.
  • Blundy, J. D., J. A. C. Robinson, and B. J. Wood (1998), Heavy REE are compatible in clinopyroxene on the spinel lherzolite solidus, Earth Planet. Sci. Lett., 160(3–4), 493504.
  • Dostal, J., C. Dupuy, J. P. Carron, M. L. Dekerneizon, and R. C. Maury (1983), Partition coefficients of trace elements: Application to volcanic rocks of St Vincent, West Indies, Geochim. Cosmochim. Acta, 47(3), 525533.
  • Foley, S. F., S. E. Jackson, B. J. Fryer, J. D. Greenough, and G. A. Jenner (1996), Trace element partition coefficients for clinopyroxene and phlogopite in an alkaline lamprophyre from Newfoundland by LAM-ICP-MS, Geochim. Cosmochim. Acta, 60(4), 629638.
  • Fujimaki, H., M. Tatsumoto, and K. Aoki (1984), Partition coefficients of Hf, Zr, and REE between phenocrysts and groundmasses, Proc. Lunar Planet. Sci. Conf. 14th, Part 2, J. Geophys. Res., 89, suppl., B662B672.
  • Ghiorso, M. S. (1985), Chemical mass transfer in magmatic processes. 1. Thermodynamic relations and numerical algorithms, Contrib. Mineral. Petrol., 90(2–3), 107120.
  • Ghiorso, M. S. (1994), Algorithms for the estimation of phase stability in heterogeneous thermodynamic systems, Geochim. Cosmochim. Acta, 58(24), 54895501.
  • Ghiorso, M. S., and R. O. Sack (1995), Chemical mass transfer in magmatic processes. 4. A revised and internally consistent thermodynamic model for the interpolation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures, Contrib. Mineral. Petrol., 119(2–3), 197212.
  • Ghiorso, M. S., M. M. Hirschmann, P. W. Reiners, and V. C. Kress III (2002), The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa, Geochem. Geophys. Geosyst., 3(5), 1030, doi:10.1029/2001GC000217.
  • Haar, L. J., J. S. Gallagher, and G. S. Kell (1984), NBS/NRC Steam Tables, Taylor and Francis, Philadelphia, Pa.
  • Hack, P. J., R. L. Nielsen, and A. D. Johnston (1994), Experimentally determined rare-earth element and Y-partitioning behavior between clinopyroxene and basaltic liquids at pressures up to 20 kbar, Chem. Geol., 117(1–4), 89105.
  • Hart, S. R., and T. Dunn (1993), Experimental cpx melt partitioning of 24 trace elements, Contrib. Mineral. Petrol., 113(1), 18.
  • Hart, S. R., and A. Zindler (1986), In search of a bulk-earth composition, Chem. Geol., 57(3–4), 247267.
  • Hauri, E. H., T. P. Wagner, and T. L. Grove (1994), Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts, Chem. Geol., 117(1–4), 149166.
  • Hirschmann, M. M., and E. M. Stolper (1996), A possible role for garnet pyroxenite in the origin of the “garnet signature” in MORB, Contrib. Mineral. Petrol., 124(2), 185208.
  • Hirschmann, M. M., M. S. Ghiorso, L. E. Wasylenki, P. D. Asimow, and E. M. Stolper (1998), Calculation of peridotite partial melting from thermodynamic models of minerals and melts. I. Review of methods and comparison with experiments, J. Petrol., 39(6), 10911115.
  • Hirschmann, M. M., T. Kogiso, M. B. Baker, and E. M. Stolper (2003), Alkalic magmas generated by partial melting of garnet pyroxenite, Geology, 31(6), 481484.
  • Hirth, G., and D. L. Kohlstedt (1996), Water in the oceanic upper mantle: Implications for rheology, melt extraction and the evolution of the lithosphere, Earth Planet. Sci. Lett., 144(1–2), 93108.
  • Johnson, K. T. M. (1998), Experimental determination of partition coefficients for rare earth and high-field-strength elements between clinopyroxene, garnet, and basaltic melt at high pressures, Contrib. Mineral. Petrol., 133(1–2), 6068.
  • Kinzler, R. J., and T. L. Grove (1992), Primary magmas of mid-ocean ridge basalts: 2. Applications, J. Geophys. Res., 97(B5), 69076926.
  • Kress, V. C., and I. S. E. Carmichael (1991), The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states, Contrib. Mineral. Petrol., 108(1–2), 8292.
  • Langmuir, C. H., C. H. Klein, and T. Plank (1992), Petrological systematics of mid-ocean ridge basalts: Constraints on melt generations beneath ocean ridges, in Mantle Flow and Melt Generation at Mid-Ocean Ridges, Geophys. Monogr. Ser., vol. 71, edited by J. Phipps Morgan, D. K. Blackman, and J. M. Sinton, pp. 183280, AGU, Washington DC.
  • McKenzie, D., and M. J. Bickle (1988), The volume and composition of melt generated by extension of the lithosphere, J. Petrol., 29(3), 625679.
  • McKenzie, D., and R. K. O'Nions (1991), Partial melt distributions from inversion of rare-earth element concentrations, J. Petrol., 32(5), 10211091.
  • McKenzie, D., and R. K. O'Nions (1995), The source regions of ocean island basalts, J. Petrol., 36(1), 133159.
  • Ohtani, E., I. Kawabe, J. Moriyama, and Y. Nagata (1989), Partitioning of elements between majorite garnet and melt and implications for petrogenesis of komatiite, Contrib. Mineral. Petrol., 103(3), 263269.
  • Pertermann, M., and M. M. Hirschmann (2003), Partial melting experiments on a MORB-like pyroxenite between 2 and 3 GPa: Constraints on the presence of pyroxenite in basalt source regions from solidus location and melting rate, J. Geophys. Res., 108(B2), 2125, doi:10.1029/2000JB000118.
  • Pertermann, M., M. M. Hirschmann, K. Hametner, D. Günther, and M. W. Schmidt (2004), Experimental determination of trace element partitioning between garnet and silica-rich liquid during anhydrous partial melting of MORB-like eclogite, Geochem. Geophys. Geosyst., 5, Q05A01, doi:10.1029/2003GC000638.
  • Pitzer, K. S., and S. M. Sterner (1994), Equations of state valid continuously from zero to extreme pressures for H2O and CO2, J. Chem. Phys., 101(4), 31113116.
  • Plank, T., M. Spiegelman, C. H. Langmuir, and D. W. Forsyth (1995), The meaning of mean F: Clarifying the mean extent of melting at ocean ridges, J. Geophys. Res., 100(B8), 15,04515,052.
  • Reid, F. (1983), Origin of the rhyolitic rocks of the Taupo Volcanic Zone, New Zealand, J. Volcanol. Geotherm. Res., 15(4), 315338.
  • Sobolev, A. V., A. A. Migdisov, and M. V. Portnyagin (1996), Incompatible element partitioning between clinopyroxene and basalt liquid revealed by the study of melt inclusions in minerals from Troodos lavas, Cyprus, Petrology, 4(3), 307317.
  • Su, Y., C. H. Langmuir, and P. D. Asimow (2003), PetroPlot: A plotting and data management tool set for Microsoft Excel, Geochem. Geophys. Geosyst., 4(3), 1030, doi:10.1029/2002GC000323.
  • van Westrenen, W., J. Blundy, and B. Wood (1999), Crystal-chemical controls on trace element partitioning between garnet and anhydrous silicate melt, Am. Mineral., 84(5–6), 838847.
  • Wood, B. J., and J. D. Blundy (1997), A predictive model for rare earth element partitioning between clinopyroxene and anhydrous silicate melt, Contrib. Mineral. Petrol., 129(2–3), 166181.
  • Wood, B. J., J. D. Blundy, and J. A. C. Robinson (1999), The role of clinopyroxene in generating U-series disequilibrium during mantle melting, Geochim. Cosmochim. Acta, 63(10), 16131620.
  • Workman, R. K., and S. R. Hart (2005), Major and trace element compositions of the depleted MORB mantle (DMM), Earth Planet. Sci. Lett., in press.
  • Yurimoto, H., and E. Ohtani (1992), Element partitioning between majorite and liquid: A secondary ion mass-spectrometric study, Geophys. Res. Lett., 19(1), 1720.