Determining the composition of C–H–O liquids following high-pressure and high-temperature diamond-trap experiments

Baker MB, Stolper EM (1994) Determining the composition of high pressure mantle melts using diamond aggregates. Geochim Cosmochim Acta 58:2811–2827

Brey GP, Green DH (1975) The role of CO2 in the genesis of olivine melilite. Contrib Miner Petrol 49:93–103

Dasgupta R, Hirschmann MM, Smith ND (2007) Partial melting experiments of peridotite CO2 at 3 GPa and genesis of alkalic ocean island basalts. J Petrol 48:2093–2124

Dvir O, Pettke T, Fumagalli P, Kessel R (2011) Fluids in the peridotite-water system up to 6 GPa and 800 °C: new experimental constrains on dehydration reactions. Contrib Miner Petrol 161:829–844

Eggler DH (1978) The effect of CO2 upon partial melting of peridotite in the system Na2O–CaO–Al2O3–MgO–SiO2–CO2 to 35 Kb with an analysis of melting in a peridotite-H2O–CO2 system. Am J Sci 278:305–343

Eggler DH, Baker DR (1982) Reduced volatiles in the system C–O–H: implications to mantle melting, fluid formation, and diamond genesis. In: Akimoto S, Manghnani MH (eds) High-pressure research in geophysics. Center for Academic Publications Japan, Tokyo, pp 237–250

Falloon TJ, Green DH (1989) The solidus of carbonated, fertile peridotite. Earth Planet Sci Lett 94:364–370

Falloon TJ, Green DH (1990) Solidus of carbonated fertile peridotite under fluid-saturated conditions. Geology 18:195–199

Green DH, Wallace ME (1988) Mantle metasomatism by ephemeral carbonatite melts. Nature 336:459–462

Hirose K (1997) Partial melt compositions of carbonated peridotite at 3 GPa and role of CO2 in alkali-basalt magma generation. Geophys Res Lett 24:2837–2840

Izraeli ES, Harris JW, Navon O (2001) Brine inclusions in diamonds: a new upper mantle fluid. Earth Planet Sci Lett 187:323–332

Kessel R, Ulmer P, Pettke T, Schmidt MW, Thompson AB (2004) A novel approach to determine high-pressure, high-temperature fluid and melt compositions using diamond-trap experiments. Am Miner 89:1078–1086

Kessel R, Ulmer P, Pettke T, Schmidt MW, Thompson AB (2005) The water basalt system at 4 to 6 GPa: phase relations and second critical endpoint in a K-free eclogite at 700 to 1400 °C. Earth Planet Sci Lett 237:873–892

Klein-BenDavid O, Izraeli ES, Hauri E, Navon O (2004) Mantle fluid evolution, a tale of one diamond. Lithos 77:243–253

Klein-BenDavid O, Pettke T, Kessel R (2011) Chromium mobility in hydrous fluids at upper mantle conditions. Lithos 125:122–130

Kushiro I, Hirose K (1992) Experimental determination of composition of melt formed by equilibrium partial melting of peridotite at high pressures using aggregates of diamond grains. Proc Japan Acad Ser B Phys Biol Sci 68:63–68

Leost I, Stachel T, Bre GP, Harris JW, Ryabchikov ID (2003) Diamond formation and source carbonation: mineral associations in diamonds from Namibia. Contrib Miner Petrol 145:15–24

Luth RW, Virgo D, Boyd FR, Wood BJ (1990) Ferric iron in mantle derived garnets: implications for thermobarometry and for the oxidation state of the mantle. Contrib Miner Petrol 104:56–72

Navon O, Hutcheon ID, Rossman GR, Wasserburg GJ (1988) Mantle-derived fluids in diamond micro-inclusions. Nature 335:784–789

Poli S, Schmidt MW (2002) Petrology of subducted slabs. Annu Rev Earth Planet Sci 30:207–235

Poli S, Franzolin E, Fumagalli P, Crottini A (2009) The transport of carbon and hydrogen in subducted oceanic crust: an experimental study to 5 GPa. Earth Planet Sci Lett 278:350–360

Schmidt MW, Poli S (1998) Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet Sci Lett 163:361–379

Schmidt MW, Ulmer P (2004) A rocking multianvil: elimination of chemical segregation in fluid-saturated high-pressure experiments. Geochim Cosmochim Acta 68:1889–1899

Schrauder M, Navon O (1994) Hydrous and carbonatitic mantle fluids in fibrous diamonds from Jwaneng, Botswana. Geochim Cosmochim Acta 58:761–771

Smith D (1987) Genesis of carbonate in pyrope from ultramafic diatremes on the Colorado Plateau, southwestern United States. Contrib Miner Petrol 97:389–396

Stalder R, Ulmer P, Thompson AB, Günther D (2001) High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions. Contrib Miner Petrol 140:607–618

Stalder R, Ulmer P, Günther D (2002) Fluids in the system forsteritephlogopite-H2O at 60 kbar. Schweiz Miner Petrol Mitt 82:15–24

Stockhert B, Duyster J, Trepmann C, Massonne HJ (2001) Microdiamond daughter crystals precipitated from supercritical COH plus silicate fluids included in garnet, Erzgebirge, Germany. Geology 29:391–394

Tomlinson EL, Jones, AP, Harris JW (2006) Co-existing fluid and silicate inclusions in mantle diamond. Earth Planet Sci Lett 250:581–595

Truckenbrodt J, Johannes W (1999) H2O loss during piston-cylinder experiments. Am Miner 84:1333–1335

Truckenbrodt J, Ziegenbein D, Johannes W (1997) Redox conditions in piston-cylinder apparatus: the different behavior of boron nitride and unfired pyrophyllite assemblies. Am Miner 82:337–344

Ulmer MP, Cruddace RG, Fenimore EE, Fritz GG, Snyder WA (1987) SPARTAN 1 X-ray observations of the Perseus cluster—comparison of the iron abundances and temperatures in the inner and outer regions of the clusters. Astrophys J 319:118–125

Wang A, Pasteris JD, Meyer HOA, Dele-Duboi ML (1996) Magnesite bearing inclusion assemblage in natural diamond. Earth Planet Sci Lett 141:293–306

Yaxley GM, Green DH (1994) Experimental demonstration of refractory carbonate-bearing eclogite and siliceous melt in the subduction regime. Earth Planet Sci Lett 128:313–325