Abstract
Supercritical fluids in rock–H2O systems have been proposed to be important agents of mass transfer in subduction zone environments. New experimental studies were conducted on the simple model granite system NaAlSi3O8 (Ab)–H2O in order to investigate phase relations and to develop the thermodynamic mixing properties between aqueous fluid (a.k.a. vapor, V) and silicate melt (a.k.a. liquid, L) at pressures (P) and temperatures (T) approaching those of critical mixing. We established liquidus and solvus phase relations by analyzing the quenched run products from piston–cylinder experiments over a range of \(P - T - X_{{{\text{H}}_{2} {\text{O}}}}\) conditions from 1.0 to 1.7 GPa, 630–1060 °C and 4–92 wt% H2O. Equations for the critical curve, solidus temperatures, albite solubility at the solidus, and vapor-saturated solidus H2O content were formulated as functions of \(P - T - X_{{{\text{H}}_{2} {\text{O}}}}\). We constructed a subregular solution model to describe the solvus curves using P and T dependent Margules coefficients (\(W_{{{\text{H}}_{2} {\text{O}}}}\) and \(W_{\text{Ab}}\)). Activities of H2O and Ab (\(a_{{{\text{H}}_{2} {\text{O}}}}\) and \(a_{\text{Ab}}\)) could be formulated using only the input at the solidus and the critical point at each pressure because of the nearly linear dependence of the parameters on T. The solvus curves were confirmed independently by means of criteria established for classification of quenched products as L, L + V, or V and are in excellent agreement with the compositions that can be calculated using the Margules coefficients. At 1.6 GPa, the H2O content at the vapor-saturated solidus is 44.5 ± 5.5 wt% and the solubility of albite at the solidus is 42.95 ± 0.99 wt%, indicating the imminent intersection of the two curves and thus a stable critical endpoint at some slightly higher pressure. We constrain the critical endpoint at 1.63 ± 0.02 GPa, 659 ± 5 °C, and a composition of ~ 44.7 wt% H2O based on the intersections of the pressure dependent solidus curves with the critical curve, the pressure dependent albite solubility curve with the vapor-saturated solidus curve. The 1.7 GPa experiments showed no evidence for liquid–vapor immiscibility across a wide range of compositions and temperatures (4–80 wt% H2O and 630–1050 °C, and furthermore, that low albite is stable in the presence of the supercritical fluid near the breakdown of albite to jadeite and quartz. These results provide a comprehensive account of the solution properties of subcritical and supercritical fluids in this model granite system at temperatures and pressures corresponding to the deep-crust regions of granite magma generation.
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References
Alberti A, Comin-Chiaramonti P (1976) The metamorphic evolution of Tromöy (arendal area-South Norway). Tschermaks Mineral Petrogr Mitteilungen 23(3):205–220
Aranovich LY, Shmupovich K, Fed’kin V (1987) The H2O and CO2 regime in regional metamorphism. Int Geol Rev 29(12):1379–1401
Aranovich L, Newton R, Manning C (2013) Brine-assisted anatexis: experimental melting in the system haplogranite–H2O–NaCl–KCl at deep-crustal conditions. Earth Planet Sci Lett 374:111–120
Audétat A, Keppler H (2004) Viscosity of fluids in subduction zones. Science 303(5657):513–516
Bartoli O, Acosta-Vigil A, Ferrero S, Cesare B (2016) Granitoid magmas preserved as melt inclusions in high-grade metamorphic rocks. Am Mineral 101(7):1543–1559
Bebout GE, Barton MD (1993) Metasomatism during subduction: products and possible paths in the Catalina Schist, California. Chem Geol 108(1–4):61–92
Behrens H (1995) Determination of water solubilities in high-viscosity melts: an experimental study on NaAlSi3O8 and KAlSi3O8 melts. Eur J Mineral 7:905–920
Blencoe JG (1992) A two-parameter Margules method for modelling the thermodynamic mixing properties of albite-water melts. Earth Environ Sci Trans R Soc Edinb 83(1–2):423–428
Boettcher A, Wyllie P (1969) Phase relationships in the system NaAlSiO4–SiO2–H2O to 35 kilobars pressure. Am J Sci 267(8):875–909
Bohlen SR, Boettcher A, Wall V (1982) The system albite–H2O–CO2: a model for melting and activities of water at high pressures. Am Mineral 67(5–6):451–462
Boyd F, England J (1963) Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobars. J Geophys Res 68(1):311–323
Bureau H, Keppler H (1999) Complete miscibility between silicate melts and hydrous fluids in the upper mantle: experimental evidence and geochemical implications. Earth Planet Sci Lett 165(2):187–196
Burnham CW (1975) Water and magmas; a mixing model. Geochim Cosmochim Acta 39(8):1077–1084
Burnham CW, Jahns RH (1962) A method for determining the solubility of water in silicate melts. Am J Sci 260(10):721–745
Chatterjee ND (1970) Synthesis and upper stability of paragonite. Contrib Mineral Petrol 27(3):244–257
Cooper LB, Ruscitto DM, Plank T, Wallace PJ, Syracuse EM, Manning CE (2012) Global variations in H2O/Ce: 1. Slab surface temperatures beneath volcanic arcs. Geochem Geophys Geosyst 13(3):1–27
Eggler DH, Kadik A (1979) The system NaAlSi3O8–H2O–CO2 to 20 kbar pressure; I, Compositional and thermodynamic relations of liquids and vapors coexisting with albite. Am Mineral 64(9–10):1036–1048
Ferrando S, Frezzotti M, Dallai L, Compagnoni R (2005) Multiphase solid inclusions in UHP rocks (Su-Lu, China): remnants of supercritical silicate-rich aqueous fluids released during continental subduction. Chem Geol 223(1–3):68–81
Gavrilenko M, Krawczynski M, Ruprecht P, Li W, Catalano JG (2019) The quench control of water estimates in convergent margin magmas. Am Mineral 104(7):936–948
Goldsmith JR, Jenkins DM (1985a) The high—low albite relations revealed by reversal of degree of order at high pressures. Am Mineral 70(9–10):911–923
Goldsmith JR, Jenkins DM (1985b) The hydrothermal melting of low and high albite. Am Mineral 70(9–10):924–933
Grove TL, Chatterjee N, Parman SW, Médard E (2006) The influence of H2O on mantle wedge melting. Earth Planet Sci Lett 249(1–2):74–89
Grove TL, Till CB, Krawczynski MJ (2012) The role of H2O in subduction zone magmatism. Annu Rev Earth Planet Sci 40:413–439
Hasalová P, Štípská P, Powell R, Schulmann K, Janoušek V, Lexa O (2008) Transforming mylonitic metagranite by open-system interactions during melt flow. J Metamorph Geol 26(1):55–80
Hayden LA, Manning CE (2011) Rutile solubility in supercritical NaAlSi3O8–H2O fluids. Chem Geol 284(1–2):74–81
Hermann J, Spandler CJ (2007) Sediment melts at sub-arc depths: an experimental study. J Petrol 49(4):717–740
Hermann J, Spandler C, Hack A, Korsakov AV (2006) Aqueous fluids and hydrous melts in high-pressure and ultra-high pressure rocks: implications for element transfer in subduction zones. Lithos 92(3–4):399–417
Hermann J, Zheng Y-F, Rubatto D (2013) Deep fluids in subducted continental crust. Elements 9(4):281–287
Hill EJ (1995) A deep crustal shear zone exposed in western Fiordland, New Zealand. Tectonics 14(5):1172–1181
Holland T, Powell R (1998) An internally consistent thermodynamic data set for phases of petrological interest. J Metamorph Geol 16(3):309–343
Huang J, Xiao Y (2015) Element mobility in mafic and felsic ultrahigh-pressure metamorphic rocks from the Dabie UHP Orogen, China: insights into supercritical liquids in continental subduction zones. Int Geol Rev 57(9–10):1103–1129
Hunt JD, Manning CE (2012) A thermodynamic model for the system SiO2–H2O near the upper critical end point based on quartz solubility experiments at 500–1100 °C and 5–20 kbar. Geochim Cosmochim Acta 86:196–213
Kawamoto T, Kanzaki M, Mibe K, Matsukage KN, Ono S (2012) Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism. Proc Natl Acad Sci 109(46):18695–18700
Kennedy G, Wasserburg G, Heard H, Newton R (1962) The upper three-phase region in the system SiO2–H2O. Am J Sci 260(7):501–521
Kessel R, Ulmer P, Pettke T, Schmidt M, Thompson A (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(3–4):873–892
Knapp W, van Vorst W (1959) Activities and structure of some melts in the system Na2SiO3–Na2Si2O5. J Am Ceram Soc 42(11):559–562
Litvinovsky B, Podladchikov YY (1993) Crustal anatexis during the influx of mantle volatiles. Lithos 30(2):93–107
Luth W (1976) Granite rocks. The evolution of crystalline rocks. Academic Press, New York, pp 333–417
Makhluf A, Newton R, Manning C (2016) Hydrous albite magmas at lower crustal pressure: new results on liquidus H2O content, solubility, and H2O activity in the system NaAlSi3O8–H2O–NaCl at 10 GPa. Contrib Mineral Petrol 171(8–9):75
Makhluf A, Newton R, Manning C (2017) H2O activity in albite melts at deep crustal PT conditions derived from melting experiments in the systems NaAlSi3O8–H2O–CO2 and NaAlSi3O8–H2O–NaCl. Petrology 25(5):449–457
Manning CE (1994) The solubility of quartz in H2O in the lower crust and upper mantle. Geochim Cosmochim Acta 58(22):4831–4839
Manning CE (2018) The influence of pressure on the properties and origins of hydrous silicate melts in Earth’s interior. In: Kono Y, Sanloup C (eds) Magmas under pressure: advances in high-pressure experiments on structure and properties of melts. Elsevier, Amsterdam, pp 83–113
Manning CE, Antignano A, Lin HA (2010) Premelting polymerization of crustal and mantle fluids, as indicated by the solubility of albite + paragonite + quartz in H2O at 1 GPa and 350–620 °C. Earth Planet Sci Lett 292:325–336
McLelland J, Morrison J, Selleck B, Cunningham B, Olson C, Schmidt K (2002) Hydrothermal alteration of late-to post-tectonic Lyon Mountain Granitic Gneiss, Adirondack Mountains, New York: origin of quartz–sillimanite segregations, quartz–albite lithologies, and associated Kiruna-type low-Ti Fe-oxide deposits. J Metamorph Geol 20(1):175–190
McMillan PF, Holloway JR (1987) Water solubility in aluminosilicate melts. Contrib Mineral Petrol 97(3):320–332
Mibe K, Kanzaki M, Kawamoto T, Matsukage KN, Fei Y, Ono S (2004) Determination of the second critical end point in silicate-H2O systems using high-pressure and high-temperature X-ray radiography. Geochim Cosmochim Acta 68(24):5189–5195
Mibe K, Kanzaki M, Kawamoto T, Matsukage KN, Fei Y, Ono S (2007) Second critical endpoint in the peridotite–H2O system. J Geophys Res Solid Earth 112(B3):103
Mibe K, Kawamoto T, Matsukage KN, Fei Y, Ono S (2011) Slab melting versus slab dehydration in subduction-zone magmatism. Proc Natl Acad Sci 108(20):8177–8182
Mourtada-Bonnefoi CC, Laporte D (2004) Kinetics of bubble nucleation in a rhyolitic melt: an experimental study of the effect of ascent rate. Earth Planet Sci Lett 218(3–4):521–537
Nakamura Y (1974) The system SiO2–H2O–H2 at 15 kbar. Carnegie Inst Wash Yearb 73:259–263
Newton RC, Manning CE (2008) Thermodynamics of SiO2–H2O fluid near the upper critical end point from quartz solubility measurements at 10 kbar. Earth Planet Sci Lett 274(1–2):241–249
Nowak M, Behrens H (1995) The speciation of water in haplogranitic glasses and melts determined by in situ near-infrared spectroscopy. Geochim Cosmochim Acta 59(16):3445–3450
Olsen SN, Marsh BD, Baumgartner LP (2004) Modelling mid-crustal migmatite terrains as feeder zones for granite plutons: the competing dynamics of melt transfer by bulk versus porous flow. Earth Environ Sci Trans R Soc Edinb 95(1–2):49–58
Paillat O, Elphick SC, Brown WL (1992) The solubility of water in NaAlSi3O8 melts: a re-examination of Ab–H2O phase relationships and critical behaviour at high pressures. Contrib Mineral Petrol 112(4):490–500
Pilet S, Hernandez J, Villemant B (2002) Evidence for high silicic melt circulation and metasomatic events in the mantle beneath alkaline provinces: the Na–Fe–augitic green-core pyroxenes in the Tertiary alkali basalts of the Cantal massif (French Massif Central). Mineral Petrol 76(1–2):39–62
Prouteau G, Scaillet B, Pichavant M, Maury R (2001) Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust. Nature 410(6825):197
Schmidt C, Wohlers A, Marquardt K, Watenphul A (2014) Experimental study on the pseudobinary H2O + NaAlSi3O8 at 600–800 °C and 0.3–2.4 GPa. Chem Geol 388:40–47
Shen AH, Keppler H (1997) Direct observation of complete miscibility in the albite–H2O system. Nature 385(6618):710
Silver L, Stolper E (1985) A thermodynamic model for hydrous silicate melts. J Geol 93(2):161–177
Silver L, Stolper E (1989) Water in albitic glasses. J Petrol 30(3):667–709
Sørensen K (1983) Growth and dynamics of the Nordre Strømfjord shear zone. J Geophys Res Solid Earth 88(B4):3419–3437
Sowerby JR, Keppler H (2002) The effect of fluorine, boron and excess sodium on the critical curve in the albite–H2O system. Contrib Mineral Petrol 143(1):32–37
Spera F (1974) A thermodynamic basis for predicting water solubilities in silicate melts and implications for the low velocity zone. Contrib Mineral Petrol 45(3):175–186
Stalder R, Ulmer P, Thompson AB, Günther D (2000) Experimental approach to constrain second critical end points in fluid/silicate systems: near-solidus fluids and melts in the system albite–H2O. Am Mineral 85(1):68–77
Stalder R, Ulmer P, Thompson A, Günther D (2001) High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions. Contrib Mineral Petrol 140(5):607–618
Stevens G, Clemens J (1993) Fluid-absent melting and the roles of fluids in the lithosphere: a slanted summary? Chem Geol 108(1–4):1–17
Stolper E (1989) Temperature dependence of the speciation of water in rhyolitic melts and glasses. Am Mineral 74(11–12):1247–1257
Till CB, Grove TL, Withers AC (2012) The beginnings of hydrous mantle wedge melting. Contrib Mineral Petrol 163(4):669–688
Truckenbrodt J, Johannes W (1999) H2O loss during piston-cylinder experiments. Am Mineral 84(9):1333–1335
Webster J, Kinzler R, Mathez E (1999) Chloride and water solubility in basalt and andesite melts and implications for magmatic degassing. Geochim Cosmochim Acta 63(5):729–738
Wickham SM, Taylor HP (1987) Stable isotope constraints on the origin and depth of penetration of hydrothermal fluids associated with Hercynian regional metamorphism and crustal anatexis in the Pyrenees. Contrib Mineral Petrol 95(3):255–268
Zeng Q, Nekvasil H (1996) An associated solution model for albite–water melts. Geochim Cosmochim Acta 60(1):59–73
Zheng Y-F, Hermann J (2014) Geochemistry of continental subduction-zone fluids. Earth Planets Space 66(1):93
Zheng Y-F, Xia Q-X, Chen R-X, Gao X-Y (2011) Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision. Earth Sci Rev 107(3–4):342–374
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This work was supported by National Science Foundation Grants EAR 1347987 and 1732256.
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Makhluf, A.R., Newton, R.C. & Manning, C.E. Experimental investigation of phase relations in the system NaAlSi3O8–H2O at high temperatures and pressures: liquidus relations, liquid–vapor mixing, and critical phenomena at deep crust–upper mantle conditions. Contrib Mineral Petrol 175, 76 (2020). https://doi.org/10.1007/s00410-020-01711-2
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DOI: https://doi.org/10.1007/s00410-020-01711-2