Abstract
Under the right circumstances, fluid-fluxed crustal melting occurs, as demonstrated by some amphibolite-facies migmatites, but the relatively low temperatures involved make this mode of formation an unsatisfactory model for most silicic magma genesis in arcs. The concept of silicic arc magma formation through either partial melting of metabasalts or fractionation of hydrous basaltic parent magmas should also be treated with scepticism, as both these processes produce sodic and moderately to strongly peraluminous liquids that are chemically unlike most arc silicic rocks and glasses. Furthermore, if the silicic magmas are formed in the deep crust, the fractionation model predicts evolved liquids with extreme H2O contents. Thus, the answer to the question posed in the title is that neither of these two models, in isolation, seems likely for the formation of the majority of the more silicic magmas in arc environments. Given the totality of the evidence, we favour models in which high-T processes dominate. These could include fluid-absent partial melting of older non-basaltic arc crust, entrainment of source-derived crystal cargos, hybridisation with mantle-derived magmas and, in some cases, crystal fractionation of andesitic magmas at shallow crustal levels.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Aitcheson SJ, Forrest AH (1994) Quantification of crustal contamination in open magmatic systems. J Petrol 35:461–488. https://doi.org/10.1093/petrology/35.2.461
Almeev R, Holtz F, Koepke J, Haase K, Devey C (2007) Depths of partial crystallization of H2O-bearing MORB: phase equilibria simulations of basalts at the MAR near Ascension Island (7–11°S). J Petrol 49:25–45. https://doi.org/10.1093/petrology/egm068
Alonso-Perez R, Müntener O, Ulmer P (2009) Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids. Contrib Mineral Petrol 157:541–558. https://doi.org/10.1007/s00410-008-0351-8
Annen C, Blundy JD, Sparks RSJ (2006) The genesis of intermediate and silicic magmas in deep crustal hot zones. J Petrol 47:505–539. https://doi.org/10.1093/petrology/egi084
Aranovich LY, Makhluf AR, Manning CE, Newton RC (2014) Dehydration melting and the relationship between granites and granulites. Precambrian Res 253:26–37. https://doi.org/10.1016/j.precamres.2014.07.004
Atherton MP (1990) The Coastal Batholith of Peru: the product of rapid recycling of “new” crust formed within rifted continental margin. Geol J 25:337–350. https://doi.org/10.1002/gj.3350250316
Atherton MP, Petford N (1993) Generation of sodium-rich magmas from newly underplated basaltic crust. Nature 362:144–146. https://doi.org/10.1038/362144a0
Austrheim H (1987) Eclogitization of lower crustal granulites by fluid migration through shear zones. Earth Planet Sci Lett 81:221–232. https://doi.org/10.1016/0012-821X(87)90158-0
Bachmann O, Bergantz GW (2006) Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies. J Volc Geotherm Res 149:85–102. https://doi.org/10.1016/j.jvolgeores.2005.06.002
Bacon CR, Bruggman PE, Christiansen RL, Clynne MA, Donnelly-Nolan JM, Hildreth W (1997) Primitive magmas at five Cascade volcanic fields: melts from hot, heterogeneous sub-arc mantle. Can Mineral 35:397–423
Barboza SA, Bergantz GW (1996) Dynamic model of dehydration melting motivated by a natural analogue: applications to the Ivrea-Verbano Zone, northern Italy. Earth Env Sci Trans R Soc Edinburgh 87:23–31. https://doi.org/10.1017/S0263593300006441
Bea F (1996) Controls on the trace element composition of crustal melts. Trans R Soc Edinburgh Earth Sci 87:33–41. https://doi.org/10.1017/S0263593300006453
Beard JS, Lofgren GE (1989) Effect of water on the composition of partial melts of greenstone and amphibolite. Science 244:195–197. https://doi.org/10.1126/science.244.4901.195
Beier C, Haase KM, Brandl PA, Krumm SH (2017) Primitive andesites from the Taupo Volcanic Zone formed by magma mixing. Contrib Mineral Petrol 172:33. https://doi.org/10.1007/s00410-017-1354-0
Blanco-Quintero IF, Lázaro C, Garcia-Casco A, Proenza JA, Rojas-Agramonte Y (2011) Barium-rich fluids and melts in a subduction environment (La Corea and Sierra del Convento mélanges, eastern Cuba). Contrib Mineral Petrol 162:395–413. https://doi.org/10.1007/s00410-010-0603-2
Blank JG, Stolper EM, Carroll MR (1993) Solubilities of carbon dioxide and water in rhyolitic melt at 850 °C and 750 bar. Earth Planet Sci Lett 119:27–36. https://doi.org/10.1016/0012-821X(93)90004-S
Blatter DL, Sisson TW, Hankins WB (2013) Crystallization of oxidized, moderately hydrous arc basalt at mid to lower-crustal pressures: implications for andesite genesis. Contrib Mineral Petrol 166:861–886. https://doi.org/10.1007/s00410-013-0920-3
Blundy J, Cashman KV, Rust A, Witham F (2010) A case for CO2-rich arc magmas. Earth Planet Sci Lett 290:289–301. https://doi.org/10.1016/j.epsl.2009.12.013
Boehnke P, Watson EB, Trail D, Harrison TM, Schmitt AK (2013) Zircon saturation re-revisited. Chem Geol 351:324–334. https://doi.org/10.1016/j.chemgeo.2013.05.028
Bonechi B, Perinelli C, Gaeta M, Tecchiato V, Granati SF (2017) Experimental constraints on amphibole stability in primitive alkaline and calc-alkaline magmas. Period Mineral 86:231–245. https://doi.org/10.2451/2017PM735
Borisov A, Aranovich L (2019) Zircon solubility in silicate melts: new experiments and probability of zircon crystallization in deeply evolved basic melts. Chem Geol 510:103–112. https://doi.org/10.1016/j.chemgeo.2019.02.019
Brown M (2001) Crustal melting and granite magmatism: key issues. Chem Earth Pt A Solid Earth Geod 26:201–212. https://doi.org/10.1016/S1464-1895(01)00047-3
Brown M, Solar GS (1998) Shear-zone systems and melts: feedback relations and self-organization in orogenic belts. J Struct Geol 20:211–227. https://doi.org/10.1016/S0191-8141(97)00068-0
Bryan SE, Ferrari L, Reiners PW, Allen CM, Petrone CM, Ramos Rosique A, Campbell IH (2008) New insights into crustal contributions to large volume rhyolite generation at the mid-Tertiary Sierra Madre Occidental Province, Mexico, revealed by U-Pb geochronology. J Petrol 49:47–77. https://doi.org/10.1093/petrology/egm070
Blatner P, Hu R-Z, Graham IJ, Houston-Eleftheriadis C (1996) Temperatures and isotopic evolution of silicic magmas, Taupo Volcanic Zone and Coromandel, New Zealand. New Zealand J Geol Geophys 39:353–362. https://doi.org/10.1080/00288306.1996.9514719
Bucholz CE, Gaetani GA, Behn MD, Shimizu N (2013) Post-entrapment modification of volatiles and oxygen fugacity in olivine-hosted melt inclusions. Earth Planet Sci Lett 374:145–155. https://doi.org/10.1016/j.epsl.2013.05.033
Bucholz CE, Jagoutz O, Schmidt MW, Sambuu O (2014) Fractional crystallization of high-K arc magmas: biotite- versus amphibole-dominated fractionation series in the Dariv Igneous Complex, Western Mongolia. Contrib Mineral Petrol 168:1–28. https://doi.org/10.1007/s00410-014-1072-9
Burnham CW (1981) The nature of multicomponent aluminosilicate melts. Phys Chem Earth 13–14:197–229. https://doi.org/10.1016/0079-1946(81)90011-2
Büsch W, Schneider G, Mehnert KR (1974) Initial melting at grain boundaries. Part II: melting in rocks of granodioritic, quartzdioritic and tonalitic composition. Neues Jb Miner Monatsh 1974:345–370
Calogero MA, Hetland EA, Lange RA (2020) High-resolution numerical modeling of heat and volatile transfer from basalt to wall rock: application to the crustal column beneath Long Valley Caldera, CA. J Geophys Res. https://doi.org/10.1029/2018JB016773
Cameron M, Bagby WC, Cameron KL (1980) Petrogenesis of voluminous mid-Tertiary ignimbrites of the Sierra Madre Occidental. Contrib Mineral Petrol 74:271–284. https://doi.org/10.1007/BF00371697
Carrington DP, Harley SL (1995) Partial melting and phase relations in high-grade metapelites—an experimental petrogenetic grid in the KFMASH system. Contrib Mineral Petrol 120:270–291. https://doi.org/10.1007/BF00306508
Cashman K, Blundy J (2013) Petrological cannibalism: the chemical and textural consequences of incremental magma body growth. Contrib Mineral Petrol 166:703–729. https://doi.org/10.1007/s00410-013-0895-0
Castro A (2014) The off-crust origin of granite batholiths. Geosci Front 5:63–75. https://doi.org/10.1016/j.gsf.2013.06.006
Castro A (2020) The dual origin of I-type granites: the contribution from experiments. In: Janoušek V, Bonin B, Collins WJ, Farina F, Bowden P (eds) Post-archean granitic rocks: petrogenetic processes and tectonic environments, geological society of London, special publication 491. Geological Society, London, pp 101–145
Castro A, Vogt K, Gerya T (2013) Generation of new continental crust by sublithospheric silicic-magma relamination in arcs: a test of Taylor’s andesite model. Gondwana Res 23:1554–1566. https://doi.org/10.1016/j.gr.2012.07.004
Cawthorn RG, Brown PA (1976) A model for the formation and crystallisation of corundum-normative calc-alkaline magmas through amphibole fractionation. J Geol 84:467–476
Cervantes P, Wallace PJ (2003) Role of H2O in subduction-zone magmatism: new insights from melt inclusions in high-Mg basalts from central Mexico. Geology 31:235–238. https://doi.org/10.1130/0091-7613(2003)031%3c0235:ROHOIS≤≥≥%3e2.0.CO;2
Cesare B, Ferrero S, Salvioli-Mariani E, Pedron D, Cavallo A (2009) “Nanogranite” and glassy inclusions: the anatectic melt in migmatites and granulites. Geology 37:627–630. https://doi.org/10.1130/G25759A.1
Chen L, Zhao Z-F (2017) Origin of continental arc andesites: the composition of source rocks is the key. J Asian Earth Sci 145:217–232. https://doi.org/10.1016/j.jseaes.2017.04.012
Clemens JD (1992) Partial melting and granulite genesis: a partisan overview. Precambrian Res 55:297–301. https://doi.org/10.1016/0301-9268(92)90029-N
Clemens JD (1993) Experimental evidence against CO2-promoted deep crustal melting. Nature 363:336–338. https://doi.org/10.1038/363336a0
Clemens JD (2003) S-type granitic magmas—petrogenetic issues, models and evidence. Earth-Sci Rev 61:1–18. https://doi.org/10.1016/s0012-8252(02)00107-1
Clemens JD, Droop GTR (1998) Fluids, P-T paths and the fates of anatectic melts in the Earth’s crust. Lithos 44:21–36. https://doi.org/10.1016/S0024-4937(98)00020-6
Clemens JD, Mawer CK (1992) Granitic magma transport by fracture propagation. Tectonophysics 204:339–360. https://doi.org/10.1016/0040-1951(92)90316-X
Clemens JD, Stevens G (2015) Comment on ‘Water-fluxed melting of the continental crust: a review’ by R. F. Weinberg and P. Hasalová. Lithos 234:100–101. https://doi.org/10.1016/j.lithos.2015.06.032
Clemens JD, Stevens G (2016) Melt segregation and magma interactions during crustal melting: Breaking out of the matrix. Earth Sci Rev 160:333–349. https://doi.org/10.1016/j.earscirev.2016.07.012
Clemens JD, Watkins JM (2001) The fluid regime of high-temperature metamorphism during granitoid magma genesis. Contrib Mineral Petrol 140:600–606. https://doi.org/10.1007/s004100000205
Clemens JD, Petford N, Mawer CK (1997) Ascent mechanisms of granitic magmas: causes and consequences. In: Holness M (ed) Deformation-enhanced fluid transport in the earth’s crust and mantle. Chapman & Hall, London, pp 144–171
Clemens JD, Stevens G, Farina F (2011) The enigmatic sources of I-type granites and the clinopyroxene-ilmenite connexion. Lithos 126:174–181. https://doi.org/10.1016/j.lithos.2011.07.004
Clemens JD, Buick IS, Stevens G (2016) Fluids, melting, granulites and granites: a commentary. Precambrian Res 278:400–404. https://doi.org/10.1016/j.precamres.2016.01.001
Clemens JD, Stevens G, Bryan SE (2020) Conditions during the formation of granitic magmas by crustal melting—hot or cold; drenched, damp or dry? Earth Sci Rev 200:102982. https://doi.org/10.1016/j.earscirev.2019.102982
Coldwell B, Clemens J, Petford N (2011) Deep crustal melting in the Peruvian Andes: felsic magma generation during delamination and uplift. Lithos 125:272–286. https://doi.org/10.1016/j.lithos.2011.02.011
Collins WJ, Huang H-Q, Jiang X (2016) Water-fluxed crustal melting produces Cordilleran batholiths. Geology 44:143–146. https://doi.org/10.1130/G37398.1
Collins WJ, Murphy JB, Johnson TE, Huang H-Q (2020) Critical role of water in the formation of continental crust. Nature Geosci 13:331–338. https://doi.org/10.1038/s41561-020-0573-6
Conrad WK, Nicholls IA, Wall VJ (1988) Water-saturated and -undersaturated melting of metaluminous and peraluminous crustal compositions at 10 kb: evidence for the origin of silicic magmas in the Taupo Volcanic Zone, New Zealand, and other occurrences. J Petrol 29:765–803. https://doi.org/10.1093/petrology/29.4.765
Cordell D, Unsworth MJ, Diaz D, Reyes-Wagner V, Currie CA, Sp H (2019) Fluid and melt pathways in the central Chilean subduction zone near the 2010 Maule earthquake (35–36°S) as inferred from magnetotelluric data. Geochem Geophys Geosyst 20:1818–1835. https://doi.org/10.1029/2018GC008167
Couzinié S, Bouilhol P, Laurent O, Marko L, Moyen J-F (2021) When zircon drowns: elusive geochronological record of water-fluxed orthogneiss melting in the Velay dome (Massif Central, France). Lithos 384–385:105938. https://doi.org/10.1016/j.lithos.2020.105938
Cribb JW, Barton M (1996) Geochemical effects of decoupled fractional crystallization and crustal assimilation. Lithos 37:293–307. https://doi.org/10.1016/0024-4937(95)00027-5
Danyushevsky LV, McNeill AW, Sobolev AV (2002) Experimental and petrological studies of melt inclusions in phenocrysts from mantle-derived magmas: an overview of techniques, advantages and complications. Chem Geol 183:5–24. https://doi.org/10.1016/S0009-2541(01)00369-2
Davidson J, Turner S, Handley H, Macpherson C, Dosseto A (2007) Amphibole “sponge” in arc crust? Geology 35:787–790. https://doi.org/10.1130/G236337A.1
DeBari SM, Coleman RG (1989) Examination of the deep levels of an island arc: evidence from the Tonsina Ultramafic-Mafic Assemblage, Tonsina, Alaska. J Geophys Res 94:4373–4391. https://doi.org/10.1029/JB094iB04p04373
Deering CD, Cole JW, Vogel TA (2011) Extraction of crystal-poor rhyolite from a hornblende-bearing intermediate mush: a case study of the caldera-forming Matahina eruption, Okataina volcanic complex. Contrib Mineral Petrol 161:129–151. https://doi.org/10.1007/s00410-010-0524-0
DePaolo DJ (1981) Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization. Earth Planet Sci Lett 53:189–202. https://doi.org/10.1016/0012-821X(81)90153-9
Dessimoz M, Müntener O, Ulmer P (2012) A case for hornblende dominated fractionation of arc magmas: the Chelan Complex (Washington Cascades). Contrib Mineral Petrol 163:567–589. https://doi.org/10.1007/s00410-011-0685-5
Dixon JE, Clague DA (2001) Volatiles in basaltic glasses from Loihi Seamount, Hawaii: evidence for a relatively dry plume component. J Petrol 42:227–254. https://doi.org/10.1093/petrology/42.3.627
Eggler DH (1972) Water-saturated and undersaturated melting relations in a Paricutin andesite and an estimate of water content in the natural magma. Contrib Mineral Petrol 34:261–271. https://doi.org/10.1007/BF00373757
Etheridge MA, Daczko NR, Chapman T, Stuart CA (2020) Mechanisms of melt extraction during lower crustal partial melting. J Metamorphic Geol. https://doi.org/10.1111/jmg.12561
Finger F, Schiller D, Lindner M, Hauzenberger C, Verner K, Zak J (2021) Ultra-high-temperature granites and a curious thermal eye in the post-collisional Variscan South Bohemian Batholith. Geology: submitted
Fischer KM, Ford HA, Abt DL, Rychert CA (2010) The lithosphere-asthenosphere boundary. Annu Rev Earth Planet Sci 38:551–575. https://doi.org/10.1146/annurev-earth-040809-152438
Gaetani GA, O’Leary JA, Shimizu N, Bucholz CE, Newville M (2012) Rapid reequilibration of H2O and oxygen fugacity in olivine-hosted melt inclusions. Geology 40:915–918. https://doi.org/10.1130/G32992.1
Gardien V, Thompson AB, Grujic D, Ulmer P (1995) Experimental melting of biotite + plagioclase + quartz ± muscovite assemblages and implications for crustal melting. J Geophys Res 100:15581–15591. https://doi.org/10.1029/95JB00916
Gardien V, Thompson AB, Ulmer P (2000) Melting of biotite + plagioclase + quartz gneisses: the role of H2O in the stability of amphibole. J Petrol 41:651–666. https://doi.org/10.1093/petrology/41.5.651
Gavrilenko M, Herzberg C, Vidito C, Carr MJ, Tenner T, Ozerov A (2016) A calcium-in-olivine geohygrometer and its application to subduction zone magmatism. J Petrol 57:1811–1832. https://doi.org/10.1093/petrology/egw062
Gavrilenko M, Krawczynski M, Ruprecht P, Li W, Catalano JG (2019) The quench control of water estimates in convergent margin magmas. Am Mineral 104:936–948. https://doi.org/10.2138/am-2019-6735
Gervasoni F, Klemme S, Rocha-Júnior ERV, Berndt J (2016) Zircon saturation in silicate melts: a new and improved model for aluminous and alkaline melts. Contrib Mineral Petrol 171:1–12. https://doi.org/10.1007/s00410-016-1227-y
Ghiorso MS, Evans BW (2008) Thermodynamics of rhombohedral oxide solid solutions and a revision of the Fe-Ti two-oxide geothermometer and oxygen-barometer. Am J Sci 308:957–1039. https://doi.org/10.2475/09.2008.01
Glazner AF (2019) The ascent of water-rich magma and decompression heating: a thermodynamic analysis. Am Mineral 104:890–896. https://doi.org/10.2138/am-2019-6925
Gómez-Tuena A, Straub SM, Zellmer GF (2013) Orogenic andesites and crustal growth, geological society special publication 385. The Geological Society Publishing House, Bath, p 414
Goranson RW (1931) The solubility of water in granite magmas. Am J Sci 22:481–502. https://doi.org/10.2475/ajs.s5-22.132.481
Gray CM, Kemp AIS (2009) The two-component model for the genesis of granitic rocks in southeastern Australia—Nature of the metasedimentary-derived and basaltic end members. Lithos 111:113–124. https://doi.org/10.1016/j.lithos.2009.04.010
Grove TL, Till CB, Krawczynski MJ (2012) The role of H2O in subduction zone magmatism. Ann Rev Earth Planet Sci 40:413–439. https://doi.org/10.1146/annurev-earth-042711-105310
Gualda GAR, Ghiorso MS (2013) Low-pressure origin of high-silica rhyolites and granites. J Geol 121:537–545. https://doi.org/10.1086/671395
Hamilton DL, Burnham CW, Osborn EF (1964) The solubility of water and effects of oxygen fugacity and water content on crystallization in mafic magmas. J Petrol 5:21–39. https://doi.org/10.1093/petrology/5.1.21
Hammerli J, Kemp AI, Shimura T, Vervoort JD, Dunkley DJ (2018) Generation of I-type granitic rocks by melting of heterogeneous lower crust. Geology 46:907–910. https://doi.org/10.1130/G45119.1
Hao L-L, Wang Q, Wyman DA, Ou Q, Dan W, Jiang Z-Q, Yang J-H, Li J, Long X-P (2016) Andesitic crustal growth via mélange partial melting: evidence from Early Cretaceous arc dioritic/andesitic rocks in southern Qiangtang, central Tibet. Geochem Geophys Geosyst 17:1641–1659. https://doi.org/10.1002/2016GC006248
Harris N, Vance D, Ayres M (2000) From sediment to granite: timescales of anatexis in the upper crust. Chem Geol 162:155–167. https://doi.org/10.1016/S0009-2541(99)00121-7
Hagen-Peter G, Cottle J (2018) Evaluating the relative roles of crustal growth versus reworking through continental arc magmatism: a case study from the Ross orogen, Antarctica. Gondwana Research 55:153–166. https://doi.org/10.1016/j.gr.2017.11.006
Harte B, Hunter RH, Kinny PD (1993) Melt geometry, movement and crystallisation, in relation to mantle dykes, veins and metasomatism. Phil Trans Rl Soc London 342:1–21. https://doi.org/10.1098/rsta.1993.0001
Hartel THD, Pattison DRM (1996) Genesis of the Kapuskasing (Ontario) migmatitic mafic granulites by dehydration melting of amphibolite: the importance of quartz to reaction progress. J Metamorphic Geol 14:591–611. https://doi.org/10.1046/j.1525-1314.1996.00404.x
Helz RT (1973) Phase relations of basalts in their melting range at PH2O = 5 kb as a function of oxygen fugacity. J Petrol 14:249–302. https://doi.org/10.1093/petrology/14.2.249
Helz RT (1976) Phase relations of basalts in their melting range at PH2O = 5 kb Part II. Melt compositions. J Petrol 17:139–193. https://doi.org/10.1093/petrology/17.2.139
Hildreth W, Moorbath S (1988) Crustal contributions to arc magmatism in the Andes of Central Chile. Contrib Mineral Petrol 98:455–489. https://doi.org/10.1007/BF00372365
Holness MB, Clemens JD (1999) Partial melting of the Appin Quartzite driven by fracture- controlled H2O infiltration in the aureole ofthe Ballachulish Igneous Complex, Scottish Highlands. Contrib Mineral Petrol 136:154–168. https://doi.org/10.1007/s004100050529
Holloway JR (1976) Fluids in the evolution of granitic magmas: consequences of finite CO2 solubility. Geol Soc Am Bull 87:1513–1518. https://doi.org/10.1130/0016-7606(1976)87%3c1513:FITEOG%3e2.0.CO;2
Holloway JR, Burnham CW (1972) Melting relations of basalt with equilibrium water pressure less than total pressure. J Petrol 13:1–29. https://doi.org/10.1093/petrology/13.1.1
Holtz F, Johannes W, Tamic N, Behrens H (2001) Maximum and minimum water contents of granitic melts generated in the crust: a reevaluation and implications. Lithos 56:1–14. https://doi.org/10.1016/S0024-4937(00)00056-6
Holtz F, Sato H, Lewis J, Behrens H, Nakada S (2005) Experimental petrology of the 1991–1995 Unzen dacite, Japan. Part I: phase relations, phase composition and pre-eruptive conditions. J Petrol 46:319–337. https://doi.org/10.1093/petrology/egh077
Hyndman RD, Currie CA, Pizzotti SP (2005) Subduction zone backarcs, mobile belts, and orogenic heat. GSA Today 15:4–10. https://doi.org/10.1130/1052-5173(2005)015%3c4:SZBMBA%3e2.0.CO;2
Iacovina K, Guild MR, Till CB (2020) Aqueous fluids are effective oxidizing agents of the mantle in subduction zones. Contrib Mineral Petrol 175:36. https://doi.org/10.1007/s00410-020-1673-4
Iwamori H (1998) Transportation of H2O and melting in subduction zones. Earth Planet Sci Lett 160:65–80. https://doi.org/10.1016/S0012-821X(98)00080-6
Jagoutz O, Klein B (2018) On the importance of crystallization-differentiation for the generation of SiO2-rich melts and the compositional build-up of arc (and continental) crust. Am J Sci 318:29–63. https://doi.org/10.2475/01.2018.03
Kawano S, Katayama I, Okazaki K (2011) Permeability anisotropy of serpentinite and fluid pathways in a subduction zone. Geology 39:939–942. https://doi.org/10.1130/G32173.1
Keay SM, Collins WJ, McCulloch MT (1997) A three-component Sr-Nd isotopic mixing model for granitoid genesis, Lachlan fold belt, eastern Australia. Geology 25:307. https://doi.org/10.1130/0091-7613(1997)025%3c0307:atcsni%3e2.3.co;2
Kelemen P, Yogodzinski GM, Scholl DW (2003) Along-strike variation in the aleutian island arc: genesis of high Mg# andesite and implications for continental crust. In: Eiler J (ed) Inside the subduction factory, geophysical monograph series, vol 138. American Geophysical Union, Washington, DC, pp 223–276
Kelemen P, Rilling JL, Parmentier EM, Mehl L, Hacker BR (2004) Thermal structure due to solid-state flow in the mantle wedge beneath arcs. In: Eiler J (ed) Inside the subduction factory, geophysical monograph series, vol 138. American Geophysical Union, pp 293–311
Kelsey DE, Clark C, Hand M (2008) Thermobarometric modelling of zircon and monazite growth in melt-bearing systems: examples using model metapelitic and metapsammitic granulites. J Metamorphic Geol 26:199–212. https://doi.org/10.1111/j.1525-1314.2007.00757.x
Keppler H (1989) The influence of the fluid phase composition on the solidus temperatures in the haplogranite system NaAlSi3O8-KAlSi3O8-SiO2-H2O-CO2. Contrib Mineral Petrol 102:321–327. https://doi.org/10.1007/BF00373725
Khitarov NI, Kadik AA (1973) Water and carbon dioxide in magmatic melts and peculiarities of the melting process. Contrib Mineral Petrol 41:205–215. https://doi.org/10.1007/BF00371031
Khitarov NI, Lebedev EB, Rengarten EV, Arsenieva RV (1959) Comparative characteristics of the solubility of water in basaltic and granitic melts. Geochemistry (geokhimiya) 5:479–492
Kovalenko VI, Naumov VB, Girnis AV, Dorofeeva VA, Yarmolyuk VV (2010) Average composition of basic magmas and mantle sources of island arcs and active continental margins estimated from the data on melt inclusions and quenched glasses of rocks. Petrology 18:3–28. https://doi.org/10.1134/S0869591110010017
Krawczynski MJ, Grove TL, Behrens H (2012) Amphibole stability in primitive arc magmas: effects of temperature, H2O content, and oxygen fugacity. Contrib Mineral Petrol 164:317–339. https://doi.org/10.1007/s00410-012-0740-x
Kress VC, Carmichael ISE (1991) The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states. Contrib Mineral Petrol 108:82–92. https://doi.org/10.1007/bf00307328
Lambert IB, Wyllie PJ (1972) Melting of gabbro (quartz eclogite) with excess water to 35 kilobars, with geological applications. J Geol 80:693–708
Lanphere MA, Cameron KL, Cameron M (1980) Sr isotopic geochemistry of voluminous rhyolitic ignimbrites and related rocks, Batopilas area, western Mexico. Nature 286:594–596. https://doi.org/10.1038/286594a0
Lee C-TA, Bachmann O (2014) How important is the role of crystal fractionation in making intermediate magmas? Insights from Zr and P systematics. Earth Planet Sci Lett 393:266–274. https://doi.org/10.1016/j.epsl.2014.02.044
Liu Y, Zhang Y (2004) H2O diffusion in dacitic melts. Chem Geol 209:327–340. https://doi.org/10.1016/j.chemgeo.2004.06.019
López S, Castro A (2001) Determination of the fluid-absent solidus and supersolidus phase relationships of MORB-derived amphibolites in the range 4–14 kbar. Am Mineral 86:1396–1403. https://doi.org/10.2138/am-2001-11-1208
Makhluf AR, Newton RC, Manning CE (2020) 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. https://doi.org/10.1007/s00410-020-01711-2
Martin H, Smithies RH, Rapp R, Moyen JF, Champion D (2005) An overview of adakite, tonalite-trondhjemite-granodiorite (TTG), and sanukitoid: relationships and some implications for crustal evolution. Lithos 79:1–24. https://doi.org/10.1016/j.lithos.2004.04.048
Mayne MJ, Moyen J-F, Stevens G, Kaislaniemi L (2016) Rcrust: a tool for calculating path-dependent open system processes and application to melt loss. J Metamorphic Geol 34:663–682. https://doi.org/10.1111/jmg.12199
Mayne MJ, Stevens G, Moyen J-F, Johnson T (2020) Performing process-oriented investigations involving mass transfer using Rcrust: a new phase equilibrium modelling tool. In: Janousek V, Bonin B, Collins WJ, Farina F, Bowden P (eds) Post-archean granitic rocks: petrogenetic processes and tectonic environments, geological society of london special publication 491. Geological Society, London, pp 209–222
Mehnert KR, Büsch W, Schneider G (1973) Initial melting at grain boundaries of quartz and feldspar in gneisses and granulites. Neues Jb Miner Monatsh 4:165–183
Melekhova E, Blundy J, Robertson R, Humphreys MCS (2015) Experimental evidence for polybaric differentiation of primitive arc basalt beneath St. Vincent Lesser Antilles. J Petrol 56:161–192. https://doi.org/10.1093/petrology/egu074
Mibe K, Kawamoto T, Matsukage KN, Fei Y, Ono S (2011) Slab melting versus slab dehydration in subduction-zone magmatism. PNAS 108:8177–8182. https://doi.org/10.1073/pnas.1010968108
Middlemost EAK (1994) Naming materials in the magma/igneous rock system. Earth-Sci Rev 37:215–224. https://doi.org/10.1016/0012-8252(94)90029-9
Milord I, Sawyer EW, Brown M (2001) Formation of diatexite migmatite and granite magma during anatexis of semi-pelitic metasedimentary rocks: An example from St. Malo. France J Petrol 42:487–505. https://doi.org/10.1093/petrology/42.3.487
Montel J-M, Vielzeuf D (1997) Partial melting of metagreywackes, Part II. Compositions of minerals and melts. Contrib Mineral Petrol 128:176–196. https://doi.org/10.1007/s004100050302
Moore LR, Gazel E, Tuohy R, Lloyd AS, Esposito R, Steele-MacInnis M, Hauri E, Wallace J, Plank T, Bodnar RJ (2015) Bubbles matter: An assessment of the contribution of vapor bubbles to melt inclusion volatile budgets. Am Mineral 100:806–823. https://doi.org/10.2138/am-2015-5036
Müntener O, Kelemen P, Grove T (2001) The role of H2O during crystallization of primitive arc magmas under uppermost mantle conditions and genesis of igneous pyroxenites: an experimental study. Contrib Mineral Petrol 141:643–658. https://doi.org/10.1007/s004100100266
Mysen B (2014) Water-melt interaction in hydrous magmatic systems at high temperature and pressure. Prog Earth Planet Sci 1:4. https://doi.org/10.1186/2197-4284-1-4
Mysen B, Richet P (2019) Silicate glasses and melts. Elsevier, Amsterdam, p 708
Nandedkar RH, Ulmer P, Müntener O (2014) Fractional crystallization of primitive, hydrous arc magmas: an experimental study at 0.7 GPa. Contrib Mineral Petrol 167:1015. https://doi.org/10.1007/s00410-014-1015-5
Newman S, Lowenstern JB (2002) VOLATILECALC: a silicate melt-H2O-CO2 solution model written in Visual Basic for excel. Comp & Geosci 28:597–604. https://doi.org/10.1016/S0098-3004(01)00081-4
Newman S, Stolper E, Stern R (2000) H2O and CO2 in magmas from the Mariana arc and back arc systems. Geochem Geophys Geosyst 1:1013. https://doi.org/10.1029/1999GC000027
O’Brien TM, Miller EL (2014) Continuous zircon growth during long-lived granulite facies metamorphism: a microtextural, U-Pb, Lu–Hf and trace element study of Caledonian rocks from the Arctic. Contrib Mineral Petrol 168:1071. https://doi.org/10.1007/s00410-014-1071-x
Patiño Douce AE, Beard JS (1996) Effects of P, f(O2) and Mg/Fe ratio on dehydration melting of model metagreywackes. J Petrol 37:999–1024. https://doi.org/10.1093/petrology/37.5.999
Patiño Douce AE, Harris N (1998) Experimental constraints on Himalayan anatexis. J Petrol 39:689–710. https://doi.org/10.1093/petroj/39.4.689
Patiño Douce AE, Johnston AD (1991) Phase-equilibria and melt productivity in the pelitic system—implications for the origin of peraluminous granitoids and aluminous granulites. Contrib Mineral Petrol 107:202–218. https://doi.org/10.1007/BF00310707
Peacock SM (1990) Fluid processes in subduction zones. Science 248:329–337
Perrin A, Goes S, Prytulak J, Davies DR, Wilson C, Kramer S (2016) Reconciling mantle wedge thermal structure with arc lava thermobarometric determinations in oceanic subduction zones. Geochem Geophys Geosyst 17:4105–4127. https://doi.org/10.1002/2016GC006527
PetDB Team T (2019) EarthChem Data-To-Go: IEDA Geochemical data for melt inclusions, version 1.0, February 2019, Accessed 10 Apr 2020, https://doi.org/10.1594/IEDA/111308
Petford N, Atherton MP (1995) Cretaceous-Tertiary volcanism and syn-subduction crustal extension in northern central Peru. In: Smellie JL (ed) Volcanism associated with extension at consuming plate margins, geological society of London special publication 81. The Geological Society, Bath, pp 233–248
Petford N, Atherton MP (1996) Na-rich partial melts from newly underplated basaltic crust: the Cordillera Blanca Batholith, Peru. J Petrol 37:1491–1521. https://doi.org/10.1093/petrology/37.6.1491
Petford N, Gallagher K (2001) Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma. Earth Planet Sci Lett 193:483–499. https://doi.org/10.1016/s0012-821x(01)00481-2
Petford N, Cruden AR, McCaffrey KJW, Vigneresse J-L (2000) Granite magma formation, transport and emplacement in the Earth’s crust. Nature 408:669–673. https://doi.org/10.1038/35047000
Petford N, Koenders MA, Clemens JD (2020) Igneous differentiation by deformation. Contrib Mineral Petrol 175:45. https://doi.org/10.1007/s00410-020-1674-3
Pickering JM, Johnston AD (1998) Fluid-absent melting behavior of a two-mica metapelite. J Petrol 39:1787–1804. https://doi.org/10.1093/petroj/39.10.1787
Plank T, Kelley KA, Zimmer MM, Hauri EH, Wallace PJ (2013) Why do mafic arc magmas contain ~4 wt% water on average? Earth Planet Sci Lett 364:168–179. https://doi.org/10.1016/j.epsl.2012.11.044
Portnyagin M, Almeev R, Matveev S, Holtz F (2008) Experimental evidence for rapid water exchange between melt inclusions in olivine and host magma. Earth Planet Sci Lett 272:541–552. https://doi.org/10.1016/j.epsl.2008.05.020
Portnyagin MV, Ponomareva VV, Zelenin EA, Bazanova LI, Pevzner MM, Plechova AA, Rogozin AN, Garbe-Schönberg D (2019) TephraKam: Geochemical database of glass compositions in tephra and welded tuffs from the Kamchatka volcanic arc (NW Pacific). Data Files. https://doi.org/10.13140/RG.2.2.23627.13606
Prouteau G, Maury RC, Scaillet B, Pichavant M (1999) Fluid-present melting of ocean crust in subduction zones. Geology 27:1111–1114. https://doi.org/10.1130/0091-7613(1999)027%3c1111:FPMOOC%3e2.3.CO;2
Rapp RP, Watson EB (1995) Dehydration melting of metabasalt at 8–32 kbar: implications for continental growth and crust-mantle recycling. J Petrol 36:891–931. https://doi.org/10.1093/petrology/36.4.891
Roberts MP, Clemens JD (1997) Correction to Roberts and Clemens (1995) “Feasibility of AFC models for the petrogenesis of calc-alkaline magma series.” Contrib Mineral Petrol 128:97–99. https://doi.org/10.1007/s004100050296
Roberts M, Finger F (1997) Do U-Pb zircon ages from granulites reflect peak metamorphic conditions? Geology 24:319–322. https://doi.org/10.1130/0091-7613(1997)025%3c0319:DUPZAF%3e2.3.CO;2
Rogers JJW, Satterfield ME, Skjerlie KP, Johnston AD (1993) Vapor-absent melting at 10 kbar of a biotite- and amphibole-bearing tonalitic gneiss: implications for the generation of A-type granites: comment and reply. Geology 21:89–90. https://doi.org/10.1130/0091-7613(1993)021%3c0089:VAMAKO%3e2.3.CO;2
Rushmer T (1991) Partial melting of 2 amphibolites—contrasting experimental results under fluid-absent conditions. Contrib Mineral Petrol 107:41–59. https://doi.org/10.1007/BF00311184
Rustoni G, Audétat A, Keppler H (2019) Experimental evidence for fluid-induced melting in subduction zones. Geochem Persp Lett 11:49–54. https://doi.org/10.7185/geochemlet.1925
Rutter MJ, Wyllie PJ (1988) Melting of vapour-absent tonalite at 10 kbar to simulate dehydration-melting in the deep crust. Nature 331:159–160. https://doi.org/10.1038/331159a0
Safonov O, Butvina V, Limanov E (2019) Phlogopite-forming reactions as indicators of metasomatism in the lithospheric mantle. Minerals 9:285. https://doi.org/10.3390/min9110685
Scaillet B, Holtz F, Pichavant M (1998) Phase equilibrium constraints on the viscosity of silicic magmas: 1 Volcanic-Plutonic Association. J Geophys Res 103:27257–27266. https://doi.org/10.1029/98JB02469
Schiller D, Finger F (2019) Application of Ti-in-zircon thermometry to granite studies: problems and possible solutions. Contrib Mineral Petrol 174:51. https://doi.org/10.1007/s00410-019-1585-3
Sen C, Dunn T (1994) Dehydration melting of a basaltic composition amphibolite at 1.5 and 2.0 GPa: implications for the origin of adakites. Contrib Mineral Petrol 117:394–409. https://doi.org/10.1007/BF00307273
Siégel C, Bryan SE, Allen CM, Gust DA (2018) Use and abuse of zircon-based thermometers: a critical review and a recommended approach to identify antecrystic zircons. Earth Sci Rev 176:87–116. https://doi.org/10.1016/j.earscirev.2017.08.011
Singh J, Johannes W (1996) Dehydration melting of tonalites. 1 Beginning of melting. Contrib Mineral Petrol 125:16–25. https://doi.org/10.1007/s004100050
Sisson TW, Ratajeski K, Hankins WB, Glazner AF (2005) Voluminous granitic magmas from common basaltic sources. Contrib Mineral Petrol 148:635–661. https://doi.org/10.1007/s00410-004-0632-9
Skjerlie KP, Johnston AD (1992) Vapor-absent melting at 10-kbar of a biotite-bearing and amphibole bearing tonalitic gneiss—implications for the generation of A-type granites. Geology 20:263–266. https://doi.org/10.1130/0091-7613(1992)020%3c0263:VAMAKO%3e2.3.CO;2
Skjerlie KP, Johnston AD (1993) Fluid-absent melting behaviour of an F-rich tonalitic gneiss at mid-crustal pressures: implications for the generation of anorogenic granites. J Petrol 34:785–815. https://doi.org/10.1093/petrology/34.4.785
Smith DJ (2014) Clinopyroxene precursors to amphibole sponge in arc crust. Nature Comms 5:4329. https://doi.org/10.1038/ncomms5329
Smith IEM, Worthington TJ, Stewart RB, Price RC, Gamble JA (2003) Felsic volcanism in the Kermadec arc, SW Pacific: crustal recycling in an oceanic setting. In: Larter RD, Leat PT (eds) Intra-oceanic subduction systems, geological society of London special publication 219. The Geological Society, London, pp 99–118
Spandler CJ, Arculus RJ, Eggins SM, Mavrogenes JA, Price RC, Reay RJ (2003) Petrogenesis of the Greenhills Complex, Southland, New Zealand: magmatic differentiation and cumulate formation at the roots of a Permian island-arc volcano. Contrib Mineral Petrol 144:703–721. https://doi.org/10.1007/s00410-002-0424-z
Spence DA, Turcotte DL (1990) Buoyancy-driven magma fracture: a mechanism for ascent through the lithosphere and the emplacement of diamonds. J Geophys Res 95:5133–5139. https://doi.org/10.1029/JB095iB04p05133
Spencer CJ, Cavosie AJ, Raub TD, Rollinson H, Jeon H, Searle MP, Miller JA, McDonald BJ, Evans NJ (2017) Evidence for melting mud in Earth’s mantle from extreme oxygen isotope signatures in zircon. Geology 45:975–978. https://doi.org/10.1130/G39402.1
Stevens G, Clemens JD (1993) Fluid-absent melting and the roles of fluids in the lithosphere: a slanted summary? Chem Geol 108:1–17. https://doi.org/10.1016/0009-2541(93)90314-9
Stevens G, Clemens JD, Droop GTR (1997) Melt production during granulite-facies anatexis: experimental data from “primitive” metasedimentary protoliths. Contrib Mineral Petrol 128:352–370. https://doi.org/10.1007/s004100050
Stolper E (1982) Water in silicate glasses: an infrared spectroscopy study. Contrib Mineral Petrol 81:1–17. https://doi.org/10.1007/BF00371154
Symington NJ, Weinberg RF, Hasalová P, Wolfram LC, Raveggi M, Armstrong RA (2014) Multiple intrusions and remelting-remobilization events in a magmatic arc: the St. Peter Suite. South Australia Geol Soc Am Bull 126:1200–1218. https://doi.org/10.1130/B30975.1
Tafur LA, Diener JFA (2020) Mineral equilibrium constraints on the feasibility of diffusive H2O-fluxed melting in the continental crust. J Metamorphic Geol. https://doi.org/10.1111/jmg.12536
Takeuchi S (2011) Preeruptive magma viscosity: an important measure of magma eruptibility. J Geophys Res 116:B10201. https://doi.org/10.1029/2011JB008243
Tamic N, Behrens H, Holtz F (2001) The solubility of H2O and CO2 in rhyolitic melts in equilibrium with a mixed CO2–H2O fluid phase. Chem Geol 172:333–347. https://doi.org/10.1016/S0009-2541(00)00324-7
Tamura Y, Tatsumi Y (2002) Remelting of an andesitic crust as a possible origin for rhyolitic magma in oceanic arcs: an example from the Izu—Bonin arc. J Petrol 43:1029–1047. https://doi.org/10.1093/petrology/43.6.1029
Tamura Y, Tani K, Chang Q, Suzuki T, Fiske RS (2006) Origin of silicic magmas and the compositional gap at Sumisu submarine caldera, Izu-Bonin arc, Japan. J Volc Geotherm Res 156:187–216. https://doi.org/10.1016/j.jvolgeores.2006.03.018
Tate MC, Norman MD, Johnson SE, Fanning CM, Anderson JL (1999) Generation of tonalite and trondhjemite by subvolcanic fractionation and partial melting in the Zarza Intrusive Complex, western Peninsular Ranges Batholith, northwestern Mexico. J Petrol 40:983–1010. https://doi.org/10.1093/petroj/40.6.983
Tatsumi Y, Sato T, Kodaira S (2015) Evolution of the Earth as an andesite planet: water, plate tectonics, and delamination of anti-continent. Earth Planets Space 67:91. https://doi.org/10.1186/s40623-015-0267-2
Taylor SR (1967) The origin and growth of continents. Tectonophysics 4:17–34. https://doi.org/10.1016/0040-1951(67)90056-X
Thomas JB, Watson EB, Spear FS, Wark DA (2015) TitaniQ recrystallized: experimental confirmation of the original Ti-in-quartz calibrations. Contrib Mineral Petrol 169:27. https://doi.org/10.1007/s00410-015-1120-0
Thompson AB (1983) Fluid-absent metamorphism. J Geol Soc London 140:533–547. https://doi.org/10.1144/gsjgs.140.4.0533
Thompson AB (1988) Dehydration melting of crustal rocks. Rend Soc Ital Mineral Petrol 43:41–60
Tuttle OF, Bowen NL (1958) Origin of granite in the light of experimental studies in the system NaAlSi3O8–KAlSi3O8–SiO2–H2O. Geol Soc Am Mem 74:153
Ulmer P, Kaegi R, Müntener O (2018) Experimentally derived intermediate to silica-rich arc magmas by fractional and equilibrium crystallization at 1·0 GPa: an evaluation of phase relationships, compositions, liquid lines of descent and oxygen fugacity. J Petrol 59:11–58. https://doi.org/10.1093/petrology/egy017
Ushioda M, Takahashi E, Hamada M, Suzuki T (2014) Water content in arc basaltic magma in the Northeast Japan and Izu arcs: an estimate from Ca/Na partitioning between plagioclase and melt. Earth Planets Space 66:127. https://doi.org/10.1186/1880-5981-66-127
Valley JW, McLelland J, Essene EJ, Lamb W (1983) Metamorphic fluids in the deep crust: evidence from the Adirondacks. Nature 301:226–228. https://doi.org/10.1038/301226a0
van der Werf T, Chatzaras V, Kriegsman LM, Kronenberg A, Tikoff B, Drury MR (2017) Constraints on the rheology of the lower crust in a strike-slip plate boundary: evidence from the San Quintín xenoliths, Baja California, Mexico. Solid Earth 8:1211–1239. https://doi.org/10.5194/se-8-1211-2017
Vielzeuf D, Clemens JD (1992) Fluid-absent melting of phlogopite + quartz: experiments and models. Am Mineral 77:1206–1222
Vielzeuf D, Holloway JR (1988) Experimental determination of the fluid-absent melting reactions in the pelitic system. Consequences for crustal differentiation. Contrib Mineral Petrol 98:257–276. https://doi.org/10.1007/BF00375178
Vielzeuf D, Montel J-M (1994) Partial melting of metagreywackes. Part I. Fluid-absent experiments and phase relationships. Contrib Mineral Petrol 117:375–393. https://doi.org/10.1007/BF00307272
Villaros A, Stevens G, Moyen J-F, Buick IS (2009) The trace element compositions of S-type granites: evidence for disequilibrium melting and accessory phase entrainment in the source. Contrib Mineral Petrol 158:543–561. https://doi.org/10.1007/s00410-009-0396-3
Vry J, Brown PE, Valley JW, Morrison J (1988) Constraints on granulite genesis from carbon isotope compositions of cordierite and graphite. Nature 332:66–68. https://doi.org/10.1038/332066a0
Wada I, Behn MD (2015) Focusing of upward fluid migration beneath volcanic arcs: effect of mineral grain size variation in the mantle wedge. Geochem Geophys Geosyst 16:3905–3923. https://doi.org/10.1002/2015GC005950
Walther JV, Orville PM (1982) Volatile production and transport in regional metamorphism. Contrib Mineral Petrol 79:252–257. https://doi.org/10.1007/BF00371516
Wark DA, Watson EB (2006) TitaniQ: a titanium-in-quartz geothermometer. Contrib Mineral Petrol 152:743–754. https://doi.org/10.1007/s00410-006-0132-1
Waters LE, Lange RA (2015) An updated calibration of the plagioclase-liquid hygrometer-thermometer applicable to basalts through rhyolites. Am Mineral 100:2172–2184. https://doi.org/10.2138/am-2015-5232
Watson EB, Harrison TM (1983) Zircon saturation revisited: temperature and compositional effects in a variety of crustal magma types. Earth Planet Sci Lett 64:295–304. https://doi.org/10.1016/0012-821X(83)90211-X
Weinberg RF, Hasalová P (2015a) Water-fluxed melting of the continental crust: a review. Lithos 212–215:158–188. https://doi.org/10.1016/j.lithos.2014.08.021
Weinberg RF, Hasalová P (2015b) Reply to comment by J.D. Clemens and G. Stevens on ‘Water-fluxed melting of the continental crust: a review.’ Lithos 234–235:102–103. https://doi.org/10.1016/j.lithos.2015.08.002
Weis FA, Skogby H, Troll VR, Deegan FM, Dahren B (2015) Magmatic water contents determined through clinopyroxene: examples from the Western Canary Islands, Spain. Geochem Geophys Geosyst 16:2127–2146. https://doi.org/10.1002/2015GC005800
Winther KT, Newton RC (1991) Experimental melting of hydrous low-K tholeiite: evidence on the origin of Archaean cratons. Bull Geol Soc Denmark 39:213–228
Wolf MB, Wyllie PJ (1994) Dehydration-melting of amphibolite at 10 kbar—the effects of temperature and time. Contrib Mineral Petrol 115:369–383. https://doi.org/10.1007/BF00320972
Xia Q-K, Bi Y, Li P, Tian W, Wei X, Chen H-L (2016) High water content in primitive continental flood basalts. Sci Rep 6:25416. https://doi.org/10.1038/srep25416
Zamboni D, Gazel E, Ryan JG, Cannatelli C, Lucchi F, Atlas ZD, Trela J, Mazza SE, De Vivo B (2016) Contrasting sediment melt and fluid signatures for magma components in the Aeolian Arc: implications for numerical modeling of subduction systems. Geochem Geophys Geosyst 17:2034–2053. https://doi.org/10.1002/2016GC006301
Zen E (1986) Aluminum enrichment in silicate melts by fractional crystallization: some mineralogic and petrographic constraints. J Petrol 27:1095–1117. https://doi.org/10.1093/petrology/27.5.1095
Zhang Y, Behrens H (2000) H2O diffusion in rhyolitic melts and glasses. Chem Geol 169:243–262. https://doi.org/10.1016/S0009-2541(99)00231-4
Acknowledgements
Gary Stevens acknowledges general financial support through his position as SARChI Chair of Experimental Petrology at Stellenbosch University. Scott Bryan provided valuable comments on an earlier draft of the manuscript, and the manuscript was reviewed by Antonio Castro, Bill Collins and Jon Blundy, and we also acknowledge useful editorial comments from Othmar Müntener. Jon Blundy is particularly thanked for steering us toward some important previous literature.
Author information
Authors and Affiliations
Corresponding author
Additional information
Communicated by Steven Reddy.
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary Information
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Clemens, J.D., Stevens, G. & Mayne, M.J. Do arc silicic magmas form by fluid-fluxed melting of older arc crust or fractionation of basaltic magmas?. Contrib Mineral Petrol 176, 44 (2021). https://doi.org/10.1007/s00410-021-01800-w
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00410-021-01800-w