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American Mineralogist

Journal of Earth and Planetary Materials

Ed. by Baker, Don / Xu, Hongwu / Swainson, Ian


IMPACT FACTOR 2017: 2.645

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Volume 102, Issue 5

Issues

A review and update of mantle thermobarometry for primitive arc magmas

Christy B. Till
Published Online: 2017-05-06 | DOI: https://doi.org/10.2138/am-2017-5783

Abstract

Erupted lavas and tephras remain among the best tools we have to ascertain the mantle processes that give rise to the compositional diversity and spatial distribution of near-primary magmas at volcanic arcs. A compilation of mantle-melt thermobarometry for natural, primitive arc magmas to date reveals published estimates vary between ∼1000−1600 °C at ∼6–50 kbar. In addition to the variability of mantle melting processes within and between different arcs, this range of conditions is the result of different methodology, such as the nature of reverse fractional crystallization calculations, the choice of thermobarometer, how magmatic H2O was quantified and its calculated effect on pressure and temperature, and choices about mantle lithology and oxygen fugacity. New and internally consistent reverse fractionation calculations and thermobarometry for a representative subset of the primitive arc samples with adequate published petrography, measured mineral and melt compositions, and constraints on pre-eruptive H2O content suggest a smaller range of global mantle-melt equilibration conditions (∼1075−1450 °C at ∼8−19 kbar) than the literature compilation. The new pressure and temperature estimates and major element modeling are consistent with a model whereby several types of primitive arc magmas, specifically hydrous calc-alkaline basalt, primitive andesite and hydrous high-MgO liquid such as boninite, first form at the location of the water-saturated mantle solidus at pressures of ∼20−35 kbar and rise into the hot core of the mantle wedge reacting with the mantle en route. Due to their re-equilibration during ascent, these hydrous magmas ultimately record the conditions in the hot, shallow nose of the mantle wedge at the end of their mantle ascent path rather than the conditions at their point of origin as often interpreted. When the mantle residue for this process is lherzolite, calcalkaline basalt is generated. When the mantle residue is harzburgite to dunite, either high-Mg primitive andesite or high-MgO liquid is generated, depending on the H2O content. A different type of primitive arc magma, specifically nominally anhydrous arc tholeiite, is generated by near-fractional decompression melting at or near the anhydrous lherzolite solidus in the upwelling back limb of corner flow at ∼25−10 kbar and is focused into the same region of the shallow mantle wedge as the hydrous melts. The similarity in the terminus of the mantle ascent paths for both wet and dry primitive arc magmas likely explains their eruption in close spatial and temporal proximity at many arcs. The conditions of last mantle equilibration for primitive arc tholeiites generated by decompression melting also imply that the convecting mantle extends to 10 kbar (∼30 km) or less below most arcs. The range of mantle-melt equilibration conditions calculated here agrees well with the range of temperatures predicted for the shallow mantle wedge beneath arcs by geodynamic models, although it suggests some subduction zones may have higher maximum temperatures at shallower depths in the wedge than originally predicted. Primitive hydrous arc magmas also constrain natural variation on the order of 200−250 °C in the maximum temperature in the hot shallow nose of the mantle wedge between arcs. Thus the new primitive magma thermobarometry presented here is useful for understanding melt migration processes and the temperature structure in the uppermost part of the mantle wedge, as well as the origin of different primitive magma types at arcs.

Keywords: Arc; subduction; primitive; barometry; thermometry; mantle; magma; lherzolite; Invited Centennial article; Review article

References cited

  • Abers, G.A., van Keken, P.E., Kneller, E.A., Ferris, A., and Stachnik, J.C. (2006) The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow. Earth and Planetary Science Letters, 241, 387–397.Google Scholar

  • Aharonov, E., Spiegelman, M., and Kelemen, P. (1997) Three-dimensional flow and reaction in porous media: Implications for the Earth’s mantle and sedimentary basins. Journal of Geophysical Research: Solid Earth, 102, 14821–14833.Google Scholar

  • Albaréde, F. (1992) How deep do common basaltic magmas form and differentiate? Journal of Geophysical Research, 97, 10997–11009.Google Scholar

  • Anderson, A.T. (1974) Evidence for a picritic, volatile-rich magma beneath Mt. Shasta, California. Journal of Petrology, 15, 243–267.Google Scholar

  • Anderson, A.T., and Wright, T.L. (1972) Phenocrysts and glass inclusions and their bearing on oxidation and mixing of basaltic magmas, Kilauea volcano, Hawaii. American Mineralogist, 57, 188–216.Google Scholar

  • Bacon, C.R., Bruggman, P.E., Christiansen, R.L., Clynne, M.A., Donnelly-Nolan, J.M., and Hildret, W. (1997) Primitive magmas at five Cascades volcanic fields: Melts from hot, heterogeneous sub-arc mantle. Canadian Mineralogist, 35, 397–424.Google Scholar

  • Baker, M.B., Grove, T.L., Kinzler, R.J., Donnellynolan, J.M., and Wandless, G.A. (1991) Origin of compositional zonation (high-alumina basalt to basaltic andesite) in the Giant Crater Lava Field, Medicine Lake Volcano, Northern California. Journal of Geophysical Research, 96, 21819–21842.Google Scholar

  • Baker, M., Grove, T.L., and Price, R. (1994) Primitive basalts and andesites from the Mt. Shasta region, N California—Products of varying melt fraction and water-content. Contributions to Mineralogy and Petrology, 118, 111–129.Google Scholar

  • Bartels, K.S., Kinzler, R.J., and Grove, T.L. (1991) High pressure phase relations of primitive high-alumina basalts from Medicine Lake volcano, northern California. Contributions to Mineralogy and Petrology, 108, 253–270.Google Scholar

  • Behn, M.D., and Grove, T.L. (2015) Melting systematics in mid-ocean ridge basalts: Application of a plagioclase-spinel melting model to global variations in major element chemistry and crustal thickness. Journal of Geophysical Research: Solid Earth, 120, 4863–4886.Google Scholar

  • Blatter, D.L., Sisson, T.W., and Hankins, W.B. (2013) Crystallization of oxidized, moderately hydrous arc basalt at mid- to lower-crustal pressures: Implications for andesite genesis. Contributions to Mineralogy and Petrology, 166, 861–886.Google Scholar

  • Bloomer, S.H., and Hawkins, J.W. (1987) Petrology and geochemistry of boninite series volcanic-rocks from the Mariana Trench. Contributions to Mineralogy and Petrology, 97, 361–377.Google Scholar

  • Bouilhol, P., Burg, J.-P., Bodinier, J.-L., Schmidt, M.W., Dawood, H., and Hussain, S. (2009) Magma and fluid percolation in arc to forearc mantle: Evidence from Sapat (Kohistan, Northern Pakistan). Lithos, 107, 17–37.Google Scholar

  • Bouvier, A.S., Metrich, N., and Deloule, E. (2008) Slab-derived fluids in the magma sources of St. Vincent (Lesser Antilles Arc): Volatile and light element imprints. Journal of Petrology, 49, 1427–1448.Google Scholar

  • Bowen, N.L., and Schairer, J.F. (1935) The system MgO-FeO-SiO2. American Journal of Science, 170, 151–217.Google Scholar

  • Brounce, M.N., Kelley, K.A., and Cottrell, E. (2014) Variations in Fe3+/Fe of Mariana Arc basalts and mantle wedge fo2. Journal of Petrology, 55, 2513–2536.Google Scholar

  • Bryant, J.A., Yogodzinski, G.M., and Churikova, T.G. (2010) High-Mg# andesitic lavas of the Shisheisky Complex, Northern Kamchatka: Implications for primitive calc-alkaline magmatism. Contributions to Mineralogy and Petrology, 161, 791–810.Google Scholar

  • Cagnioncle, A.-M., Parmentier, E.M., and Elkins-Tanton, L.T. (2007) Effect of solid flow above a subducting slab on water distribution and melting at convergent plate boundaries. Journal of Geophysical Research, 112, 1–19.Google Scholar

  • Cameron, W.E., McCulloch, M.T., and Walker, D.A. (1983) Boninite petrogenesis: chemical and Nd-Sr isotopic constraints. Earth and Planetary Science Letters, 65, 75–89.Google Scholar

  • Dietrich, V., Emmermann, R., Oberhänsli, R., and Puchelt, H. (1978) Geochemistry of basaltic and gabbroic rocks from the West Mariana Basin and the Mariana Trench. Earth and Planetary Science Letters, 39, 127–144.Google Scholar

  • Draper, D.S., and Johnston, A.D. (1992) Anhydrous PT phase relations of an Aleutian high-MgO basalt: An investigation of the role of olivine-liquid reaction in the generation of arc high-alumina basalts. Contributions to Mineralogy and Petrology, 112, 501–519.Google Scholar

  • Elkins-Tanton, L.T., Grove, T.L., and Donnelly-Nolan, J. (2001) Hot, shallow mantle melting under the Cascades volcanic arc. Geology, 29, 631–634.Google Scholar

  • Falloon, T., and Danyushevsky, L. (2000) Melting of refractory mantle at 1.5, 2 and 2.5 GPa under, anhydrous and H2O-undersaturated conditions: Implications for the petrogenesis of high-Ca boninites and the influence of subduction components on mantle melting. Journal of Petrology, 41, 257–283.Google Scholar

  • Ford, C.E., Russell, D.G., Craven, J.A., and Fisk, M.R. (1983) Olivine liquid equilibria - temperature, pressure and composition dependence of the crystal liquid cation partition-coefficients for Mg, Fe2+, Ca and Mn. Journal of Petrology, 24, 256–265.Google Scholar

  • Frost, D.J., and McCammon, C.A. (2008) The redox state of Earth’s mantle. Annual Review of Earth and Planetary Sciences, 36, 389–420.Google Scholar

  • Gaetani, G.A., and Grove, T.L. (1998) The influence of water on melting of mantle peridotite. Contributions to Mineralogy and Petrology, 131, 323–346.Google Scholar

  • Gamble, J.A., Smith, I., Graham, I.J., and Kokelaar, B.P. (1990) The petrology, phase relations and tectonic setting of basalts from the Taupo Volcanic Zone, New Zealand and the Kermadec Island Arc-Havre Trough, SW Pacific. Journal of Volcanology and Geothermal Research, 43, 253–270.Google Scholar

  • Gerya, T.V., Stöckhert, B., and Perchuk, A.L. (2002) Exhumation of high-pressure metamorphic rocks in a subduction channel: A numerical simulation. Tectonics, 21, 6-1-6-19.Google Scholar

  • Green, D.H. (1973) Experimental melting studies on a model upper mantle composition at high-pressure under water-saturated and water-undersaturated conditions. Earth and Planetary Science Letters, 19, 37–53.Google Scholar

  • Grove, T.L. (1993) Corrections to expressions for calculating mineral components in “Origin of Calc-Alkaline Series Lavas at Medicine Lake Volcano by Fractionation, Assimilation and Mixing” and “Experimental Petrology of normal MORB near Kane Fracture Zone: 22°–25°N, mid-Atlantic ridge.” Contributions to Mineralogy and Petrology, 114, 422–424.Google Scholar

  • Grove, T.L., and Juster, T.C. (1989) Experimental investigations of low-Ca pyroxene stability and olivine pyroxene liquid equilibria at 1-atm in natural basaltic and andesitic liquids. Contributions to Mineralogy and Petrology, 103, 287–305.Google Scholar

  • Grove, T.L., Kinzler, R.J., and Bryan, W.B. (1992) Fractionation of mid-ocean ridge basalt (MORB). In Mantle Flow and Melt Generation at Mid-Ocean Ridges, 71, 281–310. American Geophysical Union, Washington, D.C.Google Scholar

  • Grove, T.L., Parman, S., Bowring, S.A., Price, R., and Baker, M. (2002) The role of an H2O-rich fluid component in the generation of primitive basaltic andesites and andesites from the Mt. Shasta region, N California. Contributions to Mineralogy and Petrology, 142, 375–396.Google Scholar

  • Grove, T.L., Elkins-Tanton, L.T., Parman, S., Chatterjee, N., Muentener, O., and Gaetani, G.A. (2003) Fractional crystallization and mantle-melting controls on calc-alkaline differentiation trends. Contributions to Mineralogy and Petrology, 145, 515–533.Google Scholar

  • Grove, T.L., Chatterjee, N., Parman, S., and Médard, E. (2006) The influence of H2O on mantle wedge melting. Earth and Planetary Science Letters, 249, 74–89.Google Scholar

  • Grove, T.L., Till, C.B., and Krawczynski, M.J. (2012) The role of H2O in subduction zone magmatism. Annual Review of Earth and Planetary Sciences, 40, 413–439.Google Scholar

  • Grove, T.L., Holbig, E.S., Barr, J.A., Till, C.B., and Krawczynski, M.J. (2013) Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite. Contributions to Mineralogy and Petrology, 166, 887–910.Google Scholar

  • Hacker, B.R. (2008) H2O subduction beyond arcs. Geochemistry, Geophysics, Geosystems, 9, 1–24.Google Scholar

  • Hamada, M., and Fujii, T. (2008) Experimental constraints on the effects of pressure and H2O on the fractional crystallization of high-Mg island arc basalt. Contributions to Mineralogy and Petrology, 155, 767–790.Google Scholar

  • Hart, S.R., and Zindler, A. (1986) In search of a bulk-Earth composition. Chemical Geology, 57, 247–267.Google Scholar

  • Heath, E., Macdonald, R., and Belkin, H. (1998) Magmagenesis at Soufriere Volcano, St. Vincent, Lesser Antilles Arc. Journal of Petrology, 39, 1721–1764.Google Scholar

  • Helz, R.T., and Thornber, C.R. (1987) Geothermometry of Kilauea Iki lava lake, Hawaii. Bulletin of Volcanology, 49, 651–668.Google Scholar

  • Hesse, M., and Grove, T.L. (2003) Absarokites from the western Mexican Volcanic Belt: constraints on mantle wedge conditions. Contributions to Mineralogy and Petrology, 146, 10–27.Google Scholar

  • Hirschmann, M.M. (2000) Mantle solidus: Experimental constraints and the effects of peridotite composition. Geochemistry, Geophysics, Geosystems, 1, 1–26.Google Scholar

  • Johnson, K.T.M., Dick, H.J.B., and Shimizu, N. (1990) Melting in the oceanic mantle: An ion microprobe study of diopsides in abyssal peridotites. Journal of Geophysical Research, 95, 2661–2678.Google Scholar

  • Kamenetsky, V.S., Sobolev, A.V., Joron, J.L., and Semet, M.P. (1995) Petrology and geochemistry of cretaceous ultramafic volcanics from Eastern Kamchatka. Journal of Petrology, 36, 637–662.Google Scholar

  • Katz, R.F., Spiegelman, M., and Langmuir, C.H. (2003) A new parameterization of hydrous mantle melting. Geochemistry, Geophysics, Geosystems, 4, 1–19.Google Scholar

  • Kawamoto, T., and Holloway, J.R. (1997) Melting temperature and partial melt chemistry of H2O-saturated mantle peridotite to 11 Gigapascals. Science, 276, 240–243.Google Scholar

  • Kelemen, P.B., Dick, H.J.B., and Quick, J.E. (1992) Formation of harzburgite by pervasive melt/rock reaction in the upper mantle. Nature, 358, 635–641.Google Scholar

  • Kelemen, P.B., Whitehead, J.A., Aharonov, E., and Jordahl, K.A. (1995) Experiments on flow focusing in soluble porous media with applications to melt extraction from the mantle. Journal of Geophysical Research, 100, 475–496.Google Scholar

  • Kelemen, P.B., Hirth, G., Shimizu, N., Spiegelman, M., and Dick, H. (1997) A review of melt migration processes in the adiabatically upwelling mantle beneath oceanic spreading ridges. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 355, 283–318.Google Scholar

  • Kelemen, P.B., Rilling, J.L., Parmentier, E.M., Mehl, L., and Hacker, B.R. (2003) Thermal structure due to solid-state flow in the mantle wedge beneath arcs. In Inside the Subduction Factory, Geophysical Monograph Series, 138, 293–311. AGU, Washington, D.C.Google Scholar

  • Kelley, K.A., and Cottrell, E. (2009) Water and the oxidation state of subduction zone magmas. Science, 325, 605–607.Google Scholar

  • Kelley, K.A., and Cottrell, E. (2012) The influence of magmatic differentiation on the oxidation state of Fe in a basaltic magma. Earth and Planetary Science Letters, 329–330, 109–121.Google Scholar

  • Kelley, K.A., Plank, T., Grove, T.L., Stolper, E.M., Newman, S., and Hauri, E. (2006) Mantle melting as a function of water content beneath back-arc basins. Journal of Geophysical Research, 111, 1–27.Google Scholar

  • Kelley, K.A., Plank, T., Newman, S., Stolper, E.M., Grove, T.L., Parman, S., and Hauri, E.H. (2010) Mantle melting as a function of water content beneath the Mariana Arc. Journal of Petrology, 51, 1711–1738.Google Scholar

  • Kent, A., and Elliott, T.R. (2002) Melt inclusions from Marianas arc lavas: Implications for the composition and formation of island arc magmas. Chemical Geology, 183, 263–286.Google Scholar

  • Kimura, J.-I., and Ariskin, A.A. (2014) Calculation of water-bearing primary basalt and estimation of source mantle conditions beneath arcs: PRIMACALC2 model for WINDOWS. Geochemistry, Geophysics, Geosystems, 15, 1494–1514.Google Scholar

  • Kimura, J.-I., Hacker, B.R., van Keken, P.E., Kawabata, H., Yoshida, T., and Stern, R.J. (2009) Arc Basalt Simulator version 2, a simulation for slab dehydration and fluid-fluxed mantle melting for arc basalts: Modeling scheme and application. Geochemistry, Geophysics, Geosystems, 10, 1–32.Google Scholar

  • Kimura, J.-I., Gill, J.B., Kunikiyo, T., Osaka, I., Shimoshioiri, Y., Katakuse, M., Kakubuchi, S., Nagao, T., Furuyama, K., Kamei, A., and others. (2014) Diverse magmatic effects of subducting a hot slab in SW Japan: Results from forward modeling. Geochemistry, Geophysics, Geosystems, 15, 691–739.Google Scholar

  • Kincaid, C., and Sacks, I. (1997) Thermal and dynamical evolution of the upper mantle in subduction zones. Journal of Geophysical Research, 102, 12295–12315.Google Scholar

  • Kinzler, R.J. (1997) Melting of mantle peridotite at pressures approaching the spinel to garnet transition: Application to mid-ocean ridge basalt petrogenesis. Journal of Geophysical Research, 102, 853–874.Google Scholar

  • Kinzler, R.J., and Grove, T.L. (1992a) Primary magmas of midocean ridge basalts 1. Experiments and methods. Journal of Geophysical Research, 97, 6885–6906.Google Scholar

  • Kinzler, R.J., and Grove, T.L. (1992b) Primary magmas of midocean ridge basalts 2. Applications. Journal of Geophysical Research, 97, 6907–6926.Google Scholar

  • Kinzler, R.J., and Grove, T.L. (1993) Corrections and further discussion of the primary magmas of mid-ocean ridge basalts, 1 and 2. Journal of Geophysical Research, 98, 22339–22347.Google Scholar

  • Kohut, E.J., Stern, R.J., Kent, A.J.R., Nielsen, R.L., Bloomer, S.H., and Leybourne, M. (2006) Evidence for adiabatic decompression melting in the Southern Mariana Arc from high-Mg lavas and melt inclusions. Contributions to Mineralogy and Petrology, 152, 201–221.Google Scholar

  • Kushiro, I. (1990) Partial melting of mantle wedge and evolution of island arc crust. Journal of Geophysical Research, 95, 15929–15939.Google Scholar

  • Kushiro, I., and Sato, H. (1978) Origin of some calc-alkalic andesites in the Japanese Islands. Bulletin Volcanologique, 41, 576–585.Google Scholar

  • Kushiro, I., Syono, Y., and Akimoto, S. (1968) Melting of a peridotite nodule at high pressures and high water pressures. Journal of Geophysical Research, B, Solid Earth and Planets, 73, 6023–6029.Google Scholar

  • Langmuir, C.H., Klein, E.M., and Plank, T. (1992) Petrological systematics of mid-ocean ridge basalts: Constraints on melt generation beneath ocean ridges. Mantle Flow and Melt Generation at Mid-Ocean Ridges, 71, 183–280. American Geophysical Union, Washington, D.C.Google Scholar

  • Lee, C.-T.A., Luffi, P., Plank, T., Dalton, H., and Leeman, W.P. (2009) Constraints on the depths and temperatures of basaltic magma generation on Earth and other terrestrial planets using new thermobarometers for mafic magmas. Earth and Planetary Science Letters, 279, 20–33.Google Scholar

  • Leeman, W.P., Lewis, J.F., Evarts, R.C., Conrey, R.M., and Streck, M.J. (2005) Petrologic constraints on the thermal structure of the Cascades arc. Journal of Volcanology and Geothermal Research, 140, 67–105.Google Scholar

  • Leeman, W.P., Schutt, D.L., and Hughes, S.S. (2009) Thermal structure beneath the Snake River Plain: Implications for the Yellowstone hotspot. Journal of Volcanology and Geothermal Research, 188, 57–67.Google Scholar

  • Li, Y.B., Kimura, J.I., Machida, S., Ishii, T., Ishiwatari, A., Maruyama, S., Qiu, H.N., Ishikawa, T., Kato, Y., Haraguchi, S., and others. (2013) High-Mg adakite and low-Ca boninite from a Bonin Fore-arc Seamount: Implications for the reaction between slab melts and depleted mantle. Journal of Petrology, 54, 1149–1175.Google Scholar

  • Mitchell, A.L., and Grove, T.L. (2015) Melting the hydrous, subarc mantle: The origin of primitive andesites, Contributions to Mineralogy and Petrology, 170, 1–23.Google Scholar

  • Mitchell, A.L., and Grove, T.L. (2016) Experiments on melt–rock reaction in the shallow mantle wedge. Contributions to Mineralogy and Petrology, 171, 1–21.Google Scholar

  • Miyashiro, A. (1974) Volcanic rock series in island arcs and active continental margins. American Journal of Science, 274, 321–355.Google Scholar

  • Morishita, T., Dilek, Y., Shallo, M., Tamura, A., and Arai, S. (2011) Insight into the uppermost mantle section of a maturing arc: The Eastern Mirdita ophiolite, Albania. Lithos, 124, 215–226.Google Scholar

  • Moussallam, Y., Oppenheimer, C., Scaillet, B., Gaillard, F., Kyle, P., Peters, N., Hartley, M., Berlo, K., and Donovan, A. (2014) Tracking the changing oxidation state of Erebus magmas, from mantle to surface, driven by magma ascent and degassing. Earth and Planetary Science Letters, 393, 200–209.Google Scholar

  • Mullen, E.K., and McCallum, I.S. (2014) Origin of basalts in a hot subduction setting: Petrological and geochemical insights from Mt. Baker, Northern Cascade Arc. Journal of Petrology, 55, 241–281.Google Scholar

  • Mullen, E.K., and Weis, D. (2015) Evidence for trench-parallel mantle flow in the northern Cascade Arc from basalt geochemistry. Earth and Planetary Science Letters, 414, 100–107.Google Scholar

  • Mysen, B.O., and Boettcher, A.L. (1975) Melting of a hydrous mantle 1. Phase Relations of natural peridotite at high-pressures and temperatures with controlled activities of water, carbon-dioxide, and hydrogen. Journal of Petrology, 16, 520–548.Google Scholar

  • Navon, O., and Stolper, E. (1987) Geochemical consequences of melt percolation: the upper mantle as a chromatographic column. The Journal of Geology, 95, 285–307.Google Scholar

  • Nisbet, E.G. (1984) The continental and oceanic crust and lithosphere in the Archaean: Isostatic, thermal, and tectonic models. Canadian Journal of Earth Sciences, 21, 1426–1441.Google Scholar

  • Parman, S.W., and Grove, T.L. (2004) Harzburgite melting with and without H2O: Experimental data and predictive modeling. Journal of Geophysical Research, 109, 1–20.Google Scholar

  • Parman, S.W., Grove, T.L., Kelley, K.A., and Plank, T. (2011) Along-arc variations in the pre-eruptive H2O contents of Mariana Arc magmas inferred from fractionation paths. Journal of Petrology, 52, 257–278.Google Scholar

  • Pearce J.A., and Parkinson I.J. (1993) Trace element models for mantle melting: Application to volcanic arc petrogenesis. In H.M. Prichard, T. Alabaster, N.B.W. Harris, and C.R. Neary, Eds., Magmatic Processes and Plate Tectonics. Geological Society, London, Special Publication, 76, 373–403.Google Scholar

  • Penniston-Dorland, S.C., Kohn, M.J., and Manning, C.E. (2015) The global range of subduction zone thermal structures from exhumed blueschists and eclogites: Rocks are hotter than models. Earth and Planetary Science Letters, 428, 243–254.Google Scholar

  • Pichavant, M., and Macdonald, R. (2007) Crystallization of primitive basaltic magmas at crustal pressures and genesis of the calc-alkaline igneous suite: experimental evidence from St Vincent, Lesser Antilles arc. Contributions to Mineralogy and Petrology, 154, 535–558.Google Scholar

  • Pichavant, M., Mysen, B.O., and Macdonald, R. (2002) Source and H2O content of high-MgO magmas in island arc settings: An experimental study of a primitive calc-alkaline basalt from St. Vincent, Lesser Antilles. Geochimica et Cosmochimica Acta, 66, 2193–2209.Google Scholar

  • Pirard, C., and Hermann, J. (2015) Focused fluid transfer through the mantle above subduction zones. Geology, 43, 915–918.Google Scholar

  • Pirard C., Hermann J., and O’Neill, H.St.C. (2013) Petrology and geochemistry of the crust–mantle boundary in a Nascent Arc, Massif du Sud Ophiolite, New Caledonia, SW Pacific. Journal Petrology 54, 1759–1792.Google Scholar

  • Poli, S., and Schmidt, M.W. (1995) H2O transport and release in subduction zones—Experimental constraints on basaltic and andesitic systems. Journal of Geophysical Research, 100, 22299–22314.Google Scholar

  • Poli, S., and Schmidt, M.W. (2002) Petrology of subducted slabs. Annual Review of Earth and Planetary Science, 30, 207–235.Google Scholar

  • Portnyagin, M., Hoernle, K., Plechov, P., Mironov, N., and Khubunaya, S. (2007) Constraints on mantle melting and composition and nature of slab components in volcanic arcs from volatiles (H2O, S, Cl, F) and trace elements in melt inclusions from the Kamchatka Arc. Earth and Planetary Science Letters, 255, 53–69.Google Scholar

  • Portnyagin, M., Almeev, R., Matveev, S., and Holtz, F. (2008) Experimental evidence for rapid water exchange between melt inclusions in olivine and host magma. Earth and Planetary Science Letters, 272, 541–552.Google Scholar

  • Putirka, K.D. (2008) Thermometers and barometers for volcanic systems. Reviews in Mineralogy and Geochemistry, 69, 61–120.Google Scholar

  • Putirka, K. (2016) Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mg exchange, and mantle potential temperature. American Mineralogist, 101, 819–840.Google Scholar

  • Putirka, K.D., Perfit, M., Ryerson, F.J., and Jackson, M.G. (2007) Ambient and excess mantle temperatures, olivine thermometry, and active vs. passive upwelling. Chemical Geology, 241, 177–206.Google Scholar

  • Rowe, M.C., Kent, A.J.R., and Nielsen, R.L. (2009) Subduction influence on oxygen fugacity and trace and volatile elements in basalts across the Cascade Volcanic Arc. Journal of Petrology, 50, 61–91.Google Scholar

  • Ruscitto, D.M., Wallace, P.J., Johnson, E.R., and Kent, A. (2010) Volatile contents of mafic magmas from cinder cones in the Central Oregon High Cascades: Implications for magma formation and mantle conditions in a hot arc. Earth and Planetary Science Letters, 298, 153–161.Google Scholar

  • Sisson, T.W., and Bronto, S. (1998) Evidence for pressure-release melting beneath magmatic arcs from basalt at Galunggung, Indonesia. Nature, 391, 883–886.Google Scholar

  • Sisson, T.W., and Grove, T.L. (1993) Experimental investigations of the role of H2O in calc-alkaline differentiation and subduction zone magmatism. Contributions to Mineralogy and Petrology, 113, 143–166.Google Scholar

  • Sobolev, A.V., and Danyushevsky, L.V. (1994) Petrology and geochemistry of boninites from the North Termination of the Tonga Trench: Constraints on the generation conditions of primary high-Ca boninite magmas. Journal of Petrology, 35, 1183–1211.Google Scholar

  • Sugawara, T. (2000) Empirical relationships between temperature, pressure, and MgO content in olivine and pyroxene saturated liquid. Journal of Geophysical Research: Solid Earth, 105, 8457–8472.Google Scholar

  • Syracuse, E.M., van Keken, P.E., and Abers, G.A. (2010) The global range of subduction zone thermal models. Physics of the Earth and Planetary Interiors, 183, 73–90.Google Scholar

  • Takahashi, E., and Kushiro, I. (1983) Melting of a dry peridotite at high pressures and basalt magma genesis. American Mineralogist, 68, 859–879.Google Scholar

  • Tatsumi, Y. (1981) Melting experiments on a high-magnesian andesite. Earth and Planetary Science Letters, 54, 357–365.Google Scholar

  • Tatsumi, Y., and Ishizaka, K. (1982) Origin of high-magnesian andesites in the Setouchi volcanic belt, southwest Japan, I. Petrographical and chemical characteristics. Earth and Planetary Science Letters, 60, 293–304.Google Scholar

  • Tatsumi, Y., and Suzuki, T. (2009) Tholeiitic vs calc-alkalic differentiation and evolution of arc crust: Constraints from melting experiments on a basalt from the Izu-Bonin-Mariana Arc. Journal of Petrology, 50, 1575–1603.Google Scholar

  • Tatsumi, Y., Sakuyama, M., Fukuyama, H., and Kushiro, I. (1983) Generation of arc basalt magmas and thermal structure of the mantle wedge in subduction zones. Journal of Geophysical Research, 88, 5815–5825.Google Scholar

  • Till, C.B., Grove, T.L., and Krawczynski, M.J. (2012a) A melting model for variably depleted and enriched lherzolite in the plagioclase and spinel stability fields. Journal of Geophysical Research, 117, 1–23.Google Scholar

  • Till, C.B., Grove, T., and Withers, A.C. (2012b) The beginnings of hydrous mantle wedge melting. Contributions to Mineralogy and Petrology, 163, 669–688.Google Scholar

  • Till, C.B., Grove, T.L., Carlson, R.W., Fouch, M.J., Donnelly-Nolan, J.M., Wagner, L. S., and Hart, W.K. (2013) Depths and temperatures of < 10.5 Ma mantle melting and the lithosphere-asthenosphere boundary below southern Oregon and northern California. Geochemistry, Geophysics, Geosystems, 15, 864–879.Google Scholar

  • Tormey, D.R., Grove, T.L., and Bryan, W.B. (1987) Experimental petrology of normal MORB near the Kane Fracture Zone: 22°–25° N, Mid-Atlantic Ridge. Contributions to Mineralogy and Petrology, 96, 121–139.Google Scholar

  • van Keken, P.E., Kiefer, B., and Peacock, S.M. (2002) High-resolution models of subduction zones: Implications for mineral dehydration reactions and the transport of water into the deep mantle. Geochemistry, Geophysics, Geosystems, 3, 1056, .CrossrefGoogle Scholar

  • van Keken, P.E., Hacker, B.R., Syracuse, E.M., and Abers, G.A. (2011) Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide. Journal of Geophysical Research, 116, 1–15.Google Scholar

  • Wada, I., and Behn, M.D. (2015) Focusing of upward fluid migration beneath volcanic arcs: Effect of mineral grain size variation in the mantle wedge. Geochemistry, Geophysics, Geosystems, 16, 3905–3923.Google Scholar

  • Wade, J.A., Plank, T., Hauri, E.H., Kelley, K.A., Roggensack, K., and Zimmer, M. (2008) Prediction of magmatic water contents via measurement of H2O in clinopyroxene phenocrysts. Geology, 36, 799.Google Scholar

  • Wagner, T.P., and Grove, T.L. (1998) Melt/harzburgite reaction in the petrogenesis of tholeiitic magma from Kilauea volcano, Hawaii. Contributions to Mineralogy and Petrology, 131, 1–12.Google Scholar

  • Waters, L.E., and Lange, R.A. (2015) An updated calibration of the plagioclase-liquid hygrometer-thermometer applicable to basalts through rhyolites. American Mineralogist, 100, 2172–2184.Google Scholar

  • Watt, S.F.L., Pyle, D.M., Mather, T.A., and Naranjo, J.A. (2013) Arc magma compositions controlled by linked thermal and chemical gradients above the subducting slab. Geophysical Research Letters, 40, 2550–2556.Google Scholar

  • Weaver, S.L., Wallace, P.J., and Johnston, A.D. (2011) A comparative study of continental vs. intraoceanic arc mantle melting: Experimentally determined phase relations of hydrous primitive melts. Earth and Planetary Science Letters, 308, 97–106.Google Scholar

  • Weber, R.M., Wallace, P.J., and Dana Johnston, A. (2011) Experimental insights into the formation of high-Mg basaltic andesites in the trans-Mexican volcanic belt. Contributions to Mineralogy and Petrology, 163, 825–840.Google Scholar

  • Wilson, C.R., Spiegelman, M., van Keken, P.E., and Hacker, B.R. (2014) Fluid flow in subduction zones: The role of solid rheology and compaction pressure. Earth and Planetary Science Letters, 401, 261–274.Google Scholar

  • Yang, H.J., Kinzler, R.J., and Grove, T.L. (1996) Experiments and models of anhydrous, basaltic olivine-plagioclase-augite saturated melts from 0.001 to 10 kbar. Contributions to Mineralogy and Petrology, 124, 1–18.Google Scholar

  • Yoder, H.S., and Tilley, C.E. (1962) Origin of basalt magmas—An experimental study of natural and synthetic rock systems. Journal of Petrology, 3, 342–532.Google Scholar

About the article

Received: 2016-03-24

Accepted: 2016-12-16

Published Online: 2017-05-06

Published in Print: 2017-05-24


Citation Information: American Mineralogist, Volume 102, Issue 5, Pages 931–947, ISSN (Online) 1945-3027, ISSN (Print) 0003-004X, DOI: https://doi.org/10.2138/am-2017-5783.

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© 2017 by Walter de Gruyter Berlin/Boston.

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