Abstract
The article presents the results of experiments at pressure 4.0 GPa and temperature 1400 °C on the influence of fluids (H2O, H2O + CO2, H2O + HCl) on the composition of restite and magma formed during the melting of the peridotite-basalt-(K, Na)2CO3 system as a model analogue of the mantle reservoir contaminated with protoliths of subducted oceanic crust. The composition of the fluid has a significant impact on the phase relations. In “dry” conditions and with H2O fluid alkaline melts of phonolite type are formed, at H2O + CO2 fluid composition—trachiandezybasalts, with H2O + HCl fluid—riodacite melts. The alkaline melts coexist with an olivine-free restite pyroxene-phlogopite composition. Critical relations between fluid and silicate melt are observed in the water-bearing system. Interaction of supercritical fluid melts with peridotite restite leads to the formation of clinopyroxene, K-amphibole, phlogopite, carbonate, quenching silicate globules. Newly formed clinopyroxene and K-amphibole are in reactionary relations with olivine, orthopyroxene and clinopyroxene of peridotite restite. The revealed effects testify to instability of olivine at melting of peridotite-basalt mixture in the presence of fluid, effective influence of fluid composition on phase composition and critical ratios.
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References
Bogatikov OA, Kovalenko VI, Sharkov EV (2010) Magmatism, tectonics, geodynamics of the Earth. Nauka, Moscow, p 615
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 165:187–196
Dasgupta R, Hirschmann MM, Dellas N (2005) The effect of bulk composition on the solidus of carbonated eclogite from partial melting experiments at 3 GPa. Contrib Mineral Petrol 149:288–305
Gorbachev NS (1990) Fluid-magma interaction in sulfide-silicate systems. Int Geol Rev 32(8):749–831
Gorbachev NS (2000) Supercritical state in the hydrous mantle: evidence from experimental study of fluid-bearing peridotite at P = 40 kbar and T = 1400 °C. Dokl Akad Nauk SSSR 370:147–150
Gorbachev NS, Kostyuk AV, Shapovalov YB, (2015a) Experimental study of the peridotite-H2O system at P = 3.8–4 GPa, T = 1000–1400 °C: critical relations and vertical zoning of the upper mantle. Dokl Earth Sci 461(2):360–363
Gorbachev NS, Kostyuk AV, Shapovalov YB (2015b) Experimental study of the basalt–carbonate–H2O system at 4 GPa and 1100–1300 °C: origin of carbonatitic and high-K silicate magmas. Dokl Earth Sci 464(2):1018–1022
Keppler H, Audetat A (2005) Fluid-mineral interaction at high pressure. Mineral behavior at extreme conditions. EMU Notes Mineral 7:225–251
Kessel R, Ulmer P, Pettke T, Schmidt MW, Thompson AB (2005) The water-basalt system at 4–6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700–1400 °C. Earth Planet Sci Lett 237:873–892
Kiseeva E, Yaksley 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. Journal of Petrol 53(4):727–759
Klein-BenDavid O, Izraeli ES, Hauri E, Navon O (2007) Fluid inclusions in diamonds from the Diavik mine, Canada and the evolution of diamond-forming fluids. Geochim Cosmochim Acta 71:723–744
Litasov KD, Ohtani E (2007) Effect of mater on the phase relations in Earth’s mantle and deep water cycle. Special paper Geol Soc of Amer 421:115–156
Litvin YuA (1991) Physical and chemical studies of the melting of the Earth’s deep matter. Nauka, Moscow, p 312
Mallik A, Dasgupta R (2012) Reaction between MORB-eclogite derived melts and fertile peridotite and generation of ocean island basalts. Earth Planet Sci Lett 329(330):97–108
Mibe K, Kanzaki M, Kawamoto T, Matsukage KN, Fei Y, Ono S (2007) Second critical endpoint in the peridotite–H2O system. J Geophys Res 112:B03201
Navon O, Hutcheon ID, Rossman GR, Wasserburg GJ (1988) Mantle–derived fluids in diamond microinclusions. Nature 335:784–789
Stalder R, Ulmer P, Thompson AB, Gunther D (2001) High pressure fluids in the system MgO–SiO2–H2O under upper mantle conditions. Contrib Miner Petrol 140:607–618
Taylor LA, Neal CR (1989) Eclogites with oceanic crustal and mantle signatures from the Bellsbank kimberlite, South Africa, part 1: mineralogy, petrography, and whole rock chemistry. J Geol 97:551–567
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
Weiss Y, Kessel R, Griffin WL, Kiflawi I, Klein–BenDavid O, Bell DR, Harris JW, Navon O (2009) A new model for the evolution of diamond–forming fluids: Evidence from microinclusion–bearing diamonds from Kankan, Guinea. Lithos 112(2):660–674
Wyllie PJ, Rhyabchikov ID (2000) Volatile components, magmas, and critical fluids in upwelling mantle. J Petrol 41:1195–1206
Yaxley GM (2000) Experimental study of the phase and melting relations of homogeneous basalt plus peridotite mixtures and implications for the petrogenesis of flood basalts. Contrib Mineral Petrol 139:326–338
Acknowledgement. The study was funded by the projects of RFBR №17-05-00930a and IEM RAS №AAAA18-118020590140
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Gorbachev, N.S., Kostyuk, A.V., Gorbachev, P.N., Nekrasov, A.N., Soultanov, D.M. (2020). Influence of C–O–H–Cl-Fluids on Melting Phase Relations of the System Peridotite-Basalt: Experiments at 4.0 GPa. In: Litvin, Y., Safonov, O. (eds) Advances in Experimental and Genetic Mineralogy. Springer Mineralogy. Springer, Cham. https://doi.org/10.1007/978-3-030-42859-4_12
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