Abstract
Carbonatite compositions resulting from melting of magnesian calcite + olivine + clinopyroxene were experimentally determined in the system CaO–MgO–SiO2–CO2–H2O as a function of temperature and bulk H2O contents at 1.0 and 1.5 GPa. The melting reaction and melt compositions were found to be highly sensitive to H-loss or -gain during experiments. We hence designed a new hydrogen-trap technique, which provided sufficient control to obtain consistent results. The nominally dry solidus temperatures at 1.0 and 1.5 GPa are 1225–1250 °C and 1275–1300 °C, respectively. At 1.0 GPa, the solidus temperature decreases with H2O increasing to 3.5 wt% (1025–1050 °C), then remains approximately constant at higher H2O concentrations. Our nominally dry solidus temperatures are up to 140 °C higher than in previous studies that did not take measures to limit hydrogen infiltration and hence suffered from H2O formation in the capsule. The near-solidus anhydrous melts have 7–8 wt% SiO2 and molar Ca/(Ca + Mg) of 0.78–0.82 (XCa). Melting temperatures decrease by as much as 200 °C with increasing \({\text{X}}_{{{\text{H}}_{{2}} {\text{O}}}}\) in the coexisting COH-fluid. Concomitantly, near-solidus melt compositions change with increasing bulk H2O from siliceous Ca-rich carbonate melts to Mg-rich silico-carbonatites with up to 27.8 wt% SiO2 and 0.55 XCa. The continuous compositional array of Ca–Mg–Si carbonatites demonstrates the efficient suppression of liquid immiscibility in the alkali-free system. Diopside crystallization was found to be sensitive to temperature and bulk water contents, limiting metasomatic transformation of carbonated upper mantle to wehrlite at 1.0–1.5 GPa to < 1175 °C and < 7 wt% bulk H2O.
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References
Bailey DK (1985) Fluids, melts, flowage and styles of eruption in alkaline ultramafic magmatism. Trans Geol Soc S Afr 88:449–457
Bailey DK (1987) Mantle metasomatism—perspective and prospect. In: Fitton JG, Upton BGJ (eds) Alkaline igneous rocks. Geological Society, London, Special Publication, vol 30, pp 1–13
Baker MB, Wyllie PJ (1990) Liquid immiscibility in a nephelinite–carbonate system at 25 kbar and implications for carbonatite origin. Nature 346:168–170
Boyd FR, England JL (1963) Some effects of pressure on phase relations in the system MgO–Al2O3–SiO2. Carnegie Inst Wash Yearb 62:121–124
Brey GP, Bulatov VK, Girnis AV (2009) Influence of water and fluorine on melting of carbonated peridotite at 6 and 10 GPa. Lithos 112:249–259
Brooker RA, Hamilton DL (1990) Three-liquid immiscibility and the origin of carbonatites. Nature 346:459
Brooker RA (1995) Carbonatite genesis: an experimental evaluation of the role of liquid immiscibility to 25 kilobars. Ph.D. thesis, University of Manchester
Brooker RA (1998) The effect of CO2 saturation on immiscibility between silicate and carbonate liquids: an experimental study. J Petrol 39:1905–1915
Brooker R, Holloway JR, Hervig R (1998) Reduction in piston-cylinder experiments: the detection of carbon infiltration into platinum capsules. Am Mineral 83:985–994
Brooker RA, Kjarsgaard BA (2011) Silicate-carbonate liquid immiscibility and phase relations in the system SiO2–Na2O–Al2O3–CaO–CO2 at 0.1–2.5 GPa with applications to carbonatite genesis. J Petrol 52:1281–1305
Chou IM (1986) Permeability of precious metals to hydrogen at 2-kb total pressure and elevated-temperatures. Am J Sci 286(8):638–658
Chou IM, Eugster HP (1978) Diffusion of hydrogen through platinum membranes at high pressures and temperatures. Geochim Cosmochim Acta 42:281–288
Coltorti M, Bonadiman C, Hinton RW, Siena F, Upton BGJ (1999) Carbonatite metasomatism of the oceanic upper mantle: evidence from clinopyroxenes and glasses in ultramafic xenoliths of Grande Comore, Indian Ocean. J Petrol 40:133–165
Dalton JA, Wood BJ (1993) The compositions of primary carbonate melts and their evolution through wallrock reaction in the mantle. Earth Planet Sci Lett 119:511–525
Dalton JA, Presnall DC (1998) The continuum of primary carbonatitic–kimberlitic melt compositions in equilibrium with lherzolite: data from the system CaO–MgO–Al2O3–SiO2–CO2 at 6 GPa. J Petrol 39:1953–1964
Dasgupta R, Hirschmann MM, Withers AC (2004) Deep global cycling of carbon constrained by the solidus of anhydrous, carbonated eclogite under upper mantle conditions. Earth Planet Sci Lett 227:73–85
Dasgupta R, Hirschmann MM, Stalker K (2006) Immiscible transition from carbonate-rich to silicate-rich melts in the 3 GPa melting interval of eclogite + CO2 and genesis of silica-undersaturated ocean island lavas. J Petrol 47:647–671
Dasgupta R, Hirschmann MM (2010) The deep carbon cycle and melting in Earth’s interior. Earth Planet Sci Lett 298:1–13
Eugster HP (1957) Heterogeneous reactions involving oxidation and reduction at high pressures and temperatures. J Chem Phys 26:1760–1761
Falloon TJ, Green DH (1989) The solidus of carbonated, fertile peridotite. Earth Planet Sci Lett 94:364–370
Freda C, Baker DR, Ottolini L (2001) Reduction of water loss from gold-palladium capsules during piston-cylinder experiments by use of pyrophyllite powder. Am Mineral 86(3):234–237
Freestone IC, Hamilton DL (1980) The role of liquid immiscibility in the genesis of carbonatites—an experimental study. Contrib Mineral Petrol 73:105–117
Gade SK, Coulter KE, Way JD (2010) Effects of fabrication technique upon material properties and permeation characteristics of palladium–gold alloy membranes for hydrogen separations. Gold Bull 43(4):287–297
Hall LJ, Brodie J, Wood BJ, Carroll MR (2004) Iron and water losses from hydrous basalts contained in Au80Pd20 capsules at high pressure and temperature. Mineral Mag 68(1):75–81
Hammouda T (2003) High-pressure melting of carbonated eclogite and experimental constraints on carbon recycling and storage in the mantle. Earth Planet Sci Lett 214:357–368
Hauri EH, Shimizu N, Dieu JJ, Hart ST (1993) Evidence for hotspot-related carbonatite metasomatism in the oceanic upper mantle. Nature 365:221–227
Hazen RM, Downs RT, Jones AP, Kah L (2013) Carbon mineralogy and crystal chemistry. Rev Mineral Geochem 75:7–46
Huebner JS (1971) Buffering techniques for hydrostatic systems at elevated pressures. In: Ulmer EC (ed) Research techniques for high pressure and high temperature. Springer, Berlin, pp 123–177
Jakobsson S (2012) Oxygen fugacity control in piston-cylinder experiments. Contrib Mineral Petrol 164:397–406
Keppler H (2003) Water solubility in carbonatite melts. Am Mineral 88:1822–1824
Kiseeva ES, Yaxley GM, Hermann J, Litasov KD, Rosenthal A, Kamenetsky VS (2012) An experimental study of carbonated eclogite at 3.5–5.5 GPa—implications for silicate and carbonate metasomatism in the cratonic mantle. J Petrol 53:727–759
Kjarsgaard BA, Hamilton DL (1988) Liquid immiscibility and the origin of alkali-poor carbonatites. Mineral Mag 52:43–55
Kjarsgaard B, Hamilton DL (1989) Carbonatite origin and diversity. Nature 338:547–548
Kjarsgaard BA (1990) Nephelinite–carbonatite genesis: experiments on liquid immiscibility in alkali silicate–carbonate systems. Ph.D. thesis, University of Manchester, England
Kjarsgaard BA (1998) Phase relations of a carbonated high-CaO nephelinite at 0.2 and 0.5 GPa. J Petrol 39(11–12):2061–2075
Knapton AG (1977) Palladium alloys for hydrogen diffusion membranes. A review of high permeability materials. Platin Met Rev 21(2):45–50
Laporte D, Toplis MJ, Seyler M, Devidal JL (2004) A new experimental technique for extracting liquids from peridotite at very low degrees of melting: application to partial melting of depleted peridotite. Contrib Mineral Petrol 146:463–484
Lee W, Wyllie PJ (1992) Liquid immiscibility between silicates and carbonates must intersect suitable liquidus field boundaries to have petrogenetic significance. In: 29th international geology congress, vol 2, p 571
Lee WJ, Wyllie PJ, Rossman GR (1994) CO2-rich glass, round calcite crystals, and no liquid immiscibility in the system CaO–SiO2–CO2 at 2.5 GPa. Am Mineral 79(11–12):1135–1144
Lee WJ, Wyllie PJ (1996) Liquid immiscibility in the join NaAlSi3O8–CaCO3 to 2.5 GPa and the origin of calciocarbonatite magmas. J Petrol 37:1125–1152
Lee WJ, Wyllie PJ (1997) Liquid immiscibility between nephelinite and carbonatite from 1.0 to 2.5 GPa compared with mantle melt compositions. Contrib Mineral Petrol 127:1–16
Lee WJ, Wyllie PJ (2000) The system CaO-MgO-SiO2–CO2 at 1 GPa, metasomatic wehrlites, and primary carbonatite magmas. Contrib Mineral Petrol 138:214–228
Lee WJ, Huang WL, Wyllie P (2000) Melts in the mantle modeled in the system CaO–MgO–SiO2–CO2 at 2.7 GPa. Contrib Mineral Petrol 138:199–213
Luth RW (1989) Natural versus experimental control of oxidation state: effects on the composition and speciation of C–O–H fluids. Am Mineral 74:50–57
Maaløe S, Wyllie PJ (1975) The join grossularite-calcite through the system CaO–Al2O3–SiO2–CO2 at 30 kilobars: crystallization range of silicates and carbonates on the liquidus. Earth Planet Sci Lett 28(2):205–208
Macdonald R, Kjarsgaard BA, Skilling IP, Davies GR, Hamilton DL, Black S (1993) Liquid immiscibility between trachyte and carbonate in ash flow tuffs from Kenya. Contrib Miner Petrol 114(2):276–287
Mann U, Schmidt MW (2015) Melting of pelitic sediments at subarc depths: 1. Flux vs. fluid-absent melting and a parameterization of melt productivity. Chem Geol 404:150–167
Manning CE (1994) The solubility of quartz in H2O in the lower crust and upper mantle. Geochim Cosmochim Acta 58:4831–4839
Martin LHJ, Schmidt MW, Mattsson HB, Guenther D (2013) Element partitioning between immiscible carbonatite and silicate melts for dry and H2O-bearing systems at 1–3 GPa. J Petrol 54:2301–2338
Neumann E-R, Wulff-Pedersen E, Pearson NJ, Spencer EA (2002) Mantle xenoliths from Tenerife (Canary Islands): evidence for reactions between mantle peridotites and silicic carbonatite melts inducing Ca metasomatism. J Petrol 43:825–857
Novella D, Keshav S (2010) Silicate melt-carbonatite liquid immiscibility reconsidered in the system CaO–MgO–Al2O3 at 2–3 GPa. In: EMPG XIII, Toulouse, conference abstracts
Novella D, Keshav S, Gudfinnsson GH, Ghosh S (2014) Melting phase relations of model carbonated peridotite from 2 to 3 GPa in the system CaO–MgO–Al2O3–SiO2–CO2 and further indication of possible unmixing between carbonatite and silicate liquids. J Geophys Res Solid Earth 119:2780–2800
Olafsson M, Eggler DH (1983) Phase relations of amphibole, amphibole–carbonate, and phlogopite–carbonate peridotite: petrologic constraints on the asthenosphere. Earth Planet Sci Lett 64:305–315
Poli S (2015) Carbon mobilized at shallow depths in subduction zones by carbonatitic liquids. Nat Geosci 8:633–636
Rudnick RL, McDonough WF, Chappell BW (1993) Carbonatite metasomatism in the northern Tanzanian mantle: petrographic and geochemical characteristics. Earth Planet Sci Lett 114:463–475
Schneider ME, Eggler DH (1986) Fluids in equilibrium with peridotite minerals: implications for mantle metasomatism. Geochim Cosmochim Acta 50:711–724
Skora S, Blundy JD, Brooker RA, Green EC, de Hoog JC, Connolly JA (2015) Hydrous phase relations and trace element partitioning behaviour in calcareous sediments at subduction-zone conditions. J Petrol 56:953–980
Thomsen TB, Schmidt MW (2008) Melting of carbonated pelites at 2.5–5.0 GPa, silicate–carbonatite liquid immiscibility, and potassium–carbon metasomatism of the mantle. Earth Planet Sci Lett 267:17–31
Tiraboschi C, Tumiati S, Sverjensky D, Pettke T, Ulmer P, Poli S (2018) Experimental determination of magnesia and silica solubilities in graphite-saturated and redox-buffered high-pressure COH fluids in equilibrium with forsterite + enstatite and magnesite + enstatite. Contrib Mineral Petrol 173(1):2
Truckenbrodt J, Johannes W (1999) H2O loss during piston-cylinder experiments. Am Mineral 84(9):1333–1335
Tsuno K, Dasgupta R (2011) Melting phase relation of nominally anhydrous, carbonated politic–eclogite at 2.5–3.0 GPa and deep cycling of sedimentary carbon. Contrib Mineral Petrol 161:743–763
Tumiati S, Fumagalli P, Tiraboschi C, Poli S (2013) An experimental study on COH-bearing peridotite up to 3.2 GPa and implications for crust–mantle recycling. J Petrol 54:453–479
Wallace ME, Green DH (1988) An experimental determination of primary carbonatite magma composition. Nature 335:343–346
Wendlandt RF, Huebner JS, Harrison WJ (1982) The redox potential of boron nitride and implications for its use as a crucible material in experimental petrology. Am Mineral 67:170–174
Wood BJ, Li J, Shahar A (2013) Carbon in the core: its influence on the properties of core and mantle. Rev Mineral Geochem 75:231–250
Wyllie PJ, Tuttle OF (1960) The system CaO–CO2–H2O and the origin of carbonatites. J Petrol 1:1–46
Wyllie PJ, Huang WL (1976) Carbonation and melting reactions in the system CaO–MgO–SiO2–CO2 at mantle pressures with geophysical and petrological applications. Contrib Mineral Petrol 54(2):79–107
Wyllie PJ (1980) The origin of kimberlite. J Geophys Res B 85:6902–6910
Yaxley GM, Crawford AJ, Green DH (1991) Evidence for carbonatite metasomatism in spinel peridotite xenoliths from western Victoria, Australia. Earth Planet Sci Lett 107:305–317
Yaxley GM, Green DH, Kamenetsky V (1998) Carbonatite metasomatism in the southeastern Australian lithosphere. J Petrol 39(11–12):1917–1930
Yaxley GM, Brey GP (2004) Phase relations of carbonate-bearing eclogite assemblages from 2.5 to 5.5 GPa: implications for petrogenesis of carbonatites. Contrib Mineral Petrol 146:606–619
Yaxley GM, Ghosh S, Kiseeva E, Mallik A, Spandler C, Thomson A, Walter M (2019) CO2-rich melts in earth. In: Orcutt B, Daniel I, Dasgupta R (eds) Deep carbon: past to present. Cambridge University Press, Cambridge, pp 129–162
Acknowledgements
This study was financed by SNF grants P2EZP2_162274 and P300P2_177798 and supported by ETH Grant 34-11-1. Financial support by the Deep Carbon Observatory for experimental consumables is acknowledged. M. De Paoli, M. Galvez and C. Liebske are thanked for a critical appraisal of an earlier version of the manuscript as well as for valuable discussions. A. Makhluf and R. Esposito are thanked for technical support in the high-pressure and EPMA lab at UCLA. R.C. Newton is gratefully acknowledged for technical support in designing the H-trap double-capsule technique and for manufacturing high-precision piston-cylinder assembly parts as well as for many insightful discussions.
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Weidendorfer, D., Manning, C.E. & Schmidt, M.W. Carbonate melts in the hydrous upper mantle. Contrib Mineral Petrol 175, 72 (2020). https://doi.org/10.1007/s00410-020-01708-x
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DOI: https://doi.org/10.1007/s00410-020-01708-x