Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-25T07:20:19.725Z Has data issue: false hasContentIssue false
  • English
  • Français

Modelling the partial melting of metasediments in a low-pressure regional contact aureole: the effect of water and whole-rock composition

Published online by Cambridge University Press:  03 December 2018

Wei-(RZ) Wang ,
Geoffrey Clarke ,
Nathan R. Daczko  and
Yue Zhao
Wei-(RZ) Wang*
Affiliation:
Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China School of Geosciences, F09, University of Sydney, Sydney, NSW 2006, Australia State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Geoffrey Clarke
Affiliation:
School of Geosciences, F09, University of Sydney, Sydney, NSW 2006, Australia
Nathan R. Daczko
Affiliation:
GEMOC ARC National Key Centre, Department of Earth and Planetary Sciences, Macquarie University, NSW 2109, Australia
Yue Zhao
Affiliation:
Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China
*
Author for correspondence: Wei-(RZ) Wang, Email: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

Low-pressure regional aureoles with steep metamorphic field gradients are critical to understanding progressive metamorphism in high-temperature metasedimentary rocks. Delicately layered pelitic and psammitic metasedimentary rocks at Mt Stafford, central Australia, record a greenschist- to granulite-facies Palaeoproterozoic regional aureole, associated with S-type granite plutons, reflecting metamorphism in the range 500–800 °C and at ∼3 kbar. The rocks experienced minimal deformation during metamorphism and partial melting. Partial melting textures evolve progressively along the steep metamorphic field gradient from the incipient stages of melting marked by cuspate grains with low dihedral angles, to melt proportions sufficient to form diatexite with schollen. Phase equilibria modelling in the NCKFMASHTO system for pelitic, semi-pelitic and high- and low-ferromagnesian psammitic samples quantitatively illustrates the dependence of partial melting on rock composition and water volume. Pelitic compositions are more fertile than psammitic compositions when the water content in the rocks is low, especially during the early stages of melting. The whole-rock ferromagnesian component additionally influences melt fertility, with ferromagnesian-rich psammite being more fertile than psammite with a lower ferromagnesian component. Subtle variations in free water content can result in obvious changes in melt volume but limited variation in melt composition. Distinct melting histories of pelitic and psammitic rocks inferred from field relationships may be partially attributed to potential differences in water volume retained to super-solidus conditions. Melt composition is more dependent on the rock composition than the variation in water content.

Keywords

melt productivity and compositionwater contentresiduummigmatite
Type
Original Article
Information
Geological Magazine , Volume 156 , Issue 8 , August 2019 , pp. 1400 - 1424
Copyright
© Cambridge University Press 2018 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Acosta-Vigil, A, London, D, Morgan, GB VI, Cesare, B, Buick, B, Hermann, J and Bartoli, O (2017) Primary crustal melt compositions: insights into the controls, mechanisms and timing of generation from kinetics experiments and melt inclusions. Lithos 286–287, 454–79.CrossRefGoogle Scholar
Barker, FF (1979) Trondhjemites: definition, environment, and hypotheses of origin. In Trondhjemites, Dacites and Related Rocks (ed. Barker, FF), pp. 1–12. Amsterdam: Elsevier.Google Scholar
Ben Othman, D, Polvé, M and Allègre, CJ (1984) Nd–Sr isotopic composition of granulites and constraints on the evolution of the lower continental crust. Nature 307, 510–5.CrossRefGoogle Scholar
Bénard, F, Moutou, P and Pichavant, M (1985) Phase relations of tourmaline leucogranites and the significance of tourmaline in silicic magmas. Journal of Geology 93, 271–91.CrossRefGoogle Scholar
Berger, A, Burri, T, Alt-Epping, P and Engi, M (2008) Tectonically controlled fluid flow and water-assisted melting in the middle crust: an example from the Central Alps. Lithos 102, 598–615.CrossRefGoogle Scholar
Blake, DH and Page, RW (1988) The Proterozoic Davenport province, central Australia: regional geology and geochronology. Precambrian Research 40–41, 329–40.CrossRefGoogle Scholar
Braun, I, Raith, M and Kumar, GRR (1996) Dehydration-melting phenomena in leptynitic gneisses and the generation of leucogranites: a case study from the Kerala Khondalite Belt, southern India. Journal of Petrology 37, 1285–305.CrossRefGoogle Scholar
Brown, M (1973) The definition of metatexis, diatexis and migmatite. Proceedings of the Geologists’ Association 84, 371–82.CrossRefGoogle Scholar
Brown, M (1994) The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens. Earth-Science Reviews 36, 83–130.CrossRefGoogle Scholar
Brown, M (2001) Orogeny, migmatites and leucogranites: a review. Proceedings of the Indian Academy of Science (Earth and Planetary Science) 110, 313–36.Google Scholar
Brown, M (2010) The spatial and temporal patterning of the deep crust and implications for the process of melt extraction. Philosophical Transactions of the Royal Society, Series A 368, 11–51.CrossRefGoogle ScholarPubMed
Brown, M (2013) Granite: from genesis to emplacement. Geological Society of America Bulletin 125, 1079–113.CrossRefGoogle Scholar
Brown, M and Korhonen, FJ (2009) Some remarks on melting and extreme metamorphism of crustal rocks. In Physics and Chemistry of the Earth’s Interior (eds Gupta, AK and Dasgupta, S), pp. 67–87. New York: Indian National Science Academy, Springer (India) Private Limited.CrossRefGoogle Scholar
Brown, M, Rushmer, T and Sawyer, EW (1995) Introduction to special section: mechanisms and consequences of melt segregation from crustal protoliths. Journal of Geophysical Research 100, 15551–63.CrossRefGoogle Scholar
Brown, CR, Yakymchuk, C, Brown, M, Fanning, CM, Korhonen, FJ, Piccoli, PM and Siddoway, CS (2016) From source to sink: petrogenesis of Cretaceous anatectic granites from the Fosdick migmatite–granite complex, West Antarctica. Journal of Petrology 57, 1241–78.CrossRefGoogle Scholar
Buick, IS, Stevens, G and Gibson, RL (2004) The role of water retention in the anatexis of metapelites in the Bushveld Complex Aureole, South Africa: an experimental study. Journal of Petrology 45, 1777–97.CrossRefGoogle Scholar
Carvalho, BB, Sawyer, EW and Janasi, VA (2016) Crustal reworking in a shear zone: transformation of metagranite to migmatite. Journal of Metamorphic Geology 34, 237–64.CrossRefGoogle Scholar
Chorlton, LB and Martin, RF (1978) The effect of boron on the granite solidus. Canadian Mineralogist 16, 239–44.Google Scholar
Clarke, GL, Collins, WJ and Vernon, RH (1990) Successive overprinting granulite facies metamorphic events in the Anmatjira Range, central Australia. Journal of Metamorphic Geology 8, 65–88.CrossRefGoogle Scholar
Clarke, GL, Fitzherbert, JA, Milan, LA, Daczko, NR and Degeling, HS (2010) Anti-clockwise P-T paths in the lower crust: an example from a kyanite-bearing regional aureole, George Sound, New Zealand. Journal of Metamorphic Geology 28, 77–96.CrossRefGoogle Scholar
Clemens, JD (2006) Melting of the continental crust: fluid regimes, melting reactions, and source-rock fertility. In Evolution and Differentiation of the Continental Crust (eds Brown, M and Rushmer, T), pp. 297–331. Cambridge: Cambridge University Press.Google Scholar
Clemens, JD and Holness, MB (2000) Textural evolution and partial melting of arkose in a contact aureole: a case study and implications. Visual Geosciences 5, 1–14.CrossRefGoogle Scholar
Clemens, JD and Vielzeuf, D (1987) Constraints on melting and magma production in the crust. Earth and Planetary Science Letters 86, 287–306.CrossRefGoogle Scholar
Coggon, R and Holland, TJB (2002) Mixing properties of phengitic micas and revised garnet-phengite thermobarometers. Journal of Metamorphic Geology 20, 683–96.CrossRefGoogle Scholar
Collins, WJ and Vernon, RH (1992) Palaeozoic arc growth, deformation and migration across the Lachlan Fold Belt, southeastern Australia. In The Palaeozoic Eastern Margin of Gondwanaland: Tectonics of the Lachlan Fold Belt, Southeastern Australia and Related Orogens (eds Fergusson, CL and Glen, RA). Tectonophysics 214, 381–400.Google Scholar
Compston, DM (1995) Time constraints on the evolution of the Tennant Creek Block, northern Australia. Precambrian Research 71, 107–29.CrossRefGoogle Scholar
Craven, SJ, Daczko, NR and Halpin, JA (2012) Thermal gradient and timing of high-T–low-P metamorphism in the Wongwibinda Metamorphic Complex, southern New England Orogen, Australia. Journal of Metamorphic Geology 30, 3–20.CrossRefGoogle Scholar
Craven, SJ, Daczko, NR and Halpin, JA (2013) High-T–low-P thermal anomalies superposed on biotite-grade rocks, Wongwibinda Metamorphic Complex, southern New England Orogen, Australia: heat advection by aqueous fluid? Australian Journal of Earth Sciences 60, 621–35.CrossRefGoogle Scholar
Droop, GTR and Brodie, KH (2012) Anatectic melt volumes in the thermal aureole of the Etive Complex, Scotland: the roles of fluid-present and fluid-absent melting. Journal of Metamorphic Geology 30, 843–64.CrossRefGoogle Scholar
Droop, GTR, Clemens, JD and Dalrymple, DJ (2003) Processes and conditions during contact anatexis, melt escape and restite formation: the Huntly Gabbro complex, NE Scotland. Journal of Petrology 44, 995–1029.CrossRefGoogle Scholar
Etheridge, MA, Wall, VJ and Cox, SF (1984) High fluid pressures during regional metamorphism and deformation: implications for mass transport and deformation mechanisms. Journal of Geophysical Research 89, 4344–58.CrossRefGoogle Scholar
Fyfe, WS (1973) The granulite facies, partial melting and the Archean crust. Philosophical Transactions of the Royal Society of London, Series A 273, 457–61.CrossRefGoogle Scholar
Genier, F, Bussy, FO, Epard, J-L and Baumgartner, L (2008) Water-assisted migmatization of metagraywackes in a Variscan shear zone, Aiguilles-Rouges massif, western Alps. Lithos 102, 575–97.CrossRefGoogle Scholar
Grant, JA (2009) THERMOCALC and experimental modelling of melting of pelite, Morton Pass, Wyoming. Journal of Metamorphic Geology 27, 571–8.CrossRefGoogle Scholar
Greenfield, JE, Clarke, GL, Bland, M and Clark, DC (1996) In-situ migmatite and hybrid diatexite at Mt Stafford, central Australia. Journal of Metamorphic Geology 14, 413–26.CrossRefGoogle Scholar
Greenfield, JE, Clarke, GL and White, RW (1998) A sequence of partial melting reactions at Mt. Stafford, central Australia. Journal of Metamorphic Geology 16, 363–78.CrossRefGoogle Scholar
Guilmette, C, Indares, A and Hébert, R (2011) High-pressure anatectic paragneisses from the Namche Barwa, Eastern Himalayan Syntaxis: textural evidence for partial melting, phase equilibria modeling and tectonic implications. Lithos 124, 66–81.CrossRefGoogle Scholar
Hanson, RB and Barton, MD (1989) Magmatism and the development of low-pressure metamorphic belts: implications from the western United States and thermal modelling. Geological Society of America Bulletin 101, 1051–65.Google Scholar
Harte, B, Hunter, RH and Kinny, PD (1993) Melt geometry, movement and crystallisation, in relation to mantle dykes, veins and metasomatism. Philosophical Transactions of the Royal Society of London, Series A 342, 1–21.Google Scholar
Harte, B, Pattison, DRM and Linklater, CM (1991) Field relations and petrography of partially melted pelitic and semi-pelitic rocks. In Equilibrium and Kinetics in Contact Metamorphism, the Ballachulish Igneous Complex and its Aureole (eds Voll, G, Töpel, J, Pattison, DRM and Seifert, F), pp. 182–210. Berlin: Springer.Google Scholar
Holland, TJB and Powell, R (1998) An internally consistent thermodynamic data set for phases of petrological interest. Journal of Metamorphic Geology 16, 309–43.CrossRefGoogle Scholar
Holland, TJB and Powell, R (2003) Activity–composition relations for phases in petrological calculations: an asymmetric multicomponent formulation. Contributions to Mineralogy and Petrology 145, 492–501.CrossRefGoogle Scholar
Holness, MB, Cesare, B and Sawyer, EW (2011) Melted rocks under the microscope: microstructures and their interpretation. Elements 7, 247–52.CrossRefGoogle Scholar
Holness, MB and Clemens, JD (1999) Partial melting of the Appin Quartzite driven by fracture-controlled H2O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands. Contributions to Mineralogy and Petrology 136, 154–68.CrossRefGoogle Scholar
Holness, MB and Sawyer, EW (2008) On the pseudomorphing of melt-filled pores during the crystallization of migmatites. Journal of Petrology 49, 1343–63.CrossRefGoogle Scholar
Holtz, F and Johannes, W (1991) Genesis of peraluminous granites I: experimental investigation of melt compositions at 3 and 5 MPa and various H2O activities. Journal of Petrology 32, 935–58.CrossRefGoogle Scholar
Johannes, W and Holtz, F (1990) Formation and composition of H2O-undersaturated granitic melts. In High-Temperature Metamorphism and Crustal Anatexis (eds Ashworth, JR and Brown, M), pp. 87–104. London: Unwin Hyman.CrossRefGoogle Scholar
Johannes, W and Holtz, F (1996) Petrogenesis and Experimental Petrology of Granitic Rocks. Berlin: Springer, 335 pp.CrossRefGoogle Scholar
Johnson, TE, Brown, M and Solar, GS (2003) Low-pressure subsolidus and suprasolidus phase equilibria in the MnNCKFMASH system: constraints on conditions of regional metamorphism in western Maine, northern Appalachians. American Mineralogist 88, 624–38.CrossRefGoogle Scholar
Johnson, TE, Hudson, N and Droop, G (2001) Melt segregation structures within the Inzie Head gneisses of the northeastern Dalradian. Scottish Journal of Geology 37, 59–72.CrossRefGoogle Scholar
Johnson, TE, White, RW and Brown, M (2011) A year in the life of an aluminous metapelite xenolith–the role of heating rates, reaction overstep, H2O retention and melt loss. Lithos 124, 132–43.CrossRefGoogle Scholar
Kalt, A, Berger, A and Blumel, P (1999) Metamorphic evolution of cordierite-bearing migmatites from the Bayerische Wald (Variscan Belt, Germany). Journal of Petrology 40, 601–27.CrossRefGoogle Scholar
Kerrick, DM (1991) Overview of contact metamorphism. Reviews in Mineralogy and Geochemistry 26, 1–12.Google Scholar
Koester, E, Pawley, AR, Fernandes, LAD, Porcher, CC and Soiani, E (2002) Experimental melting of cordierite gneiss and the petrogenesis of syntranscurrent peraluminous granites in southern Brazil. Journal of Petrology 43, 1595–616.CrossRefGoogle Scholar
Laporte, D, Rapa, Ille C and Provost, A (1997) Wetting angles, equilibrium melt geometry, and the permeability threshold of partially molten crustal protoliths. In Granite: From Segregation of Melt to Emplacement Fabrics (eds Bouchez, JL, Hutton, DHW and Stephens, WE), pp. 31–54. Dordrecht: Kluwer.CrossRefGoogle Scholar
Le Breton, N and Thompson, AB (1988) Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexis. Contributions to Mineralogy and Petrology 99, 226–37.CrossRefGoogle Scholar
Marchildon, N and Brown, M (2002) Grain-scale melt distribution in two contact aureole rocks: implications for controls on melt localisation and deformation. Journal of Metamorphic Geology 20, 381–96.CrossRefGoogle Scholar
McKenzie, D (1984) The generation and compaction of partially molten rock. Journal of Petrology 25, 713–65.CrossRefGoogle Scholar
Mehnert, KR (1968) Migmatites and the Origin of Granitic Rocks. Amsterdam: Elsevier, 393 pp.Google Scholar
Noakes, LC (1953) The structure of the Northern Territory with relation to mineralization. In Geology of Australian Ore Deposits. Fifth Empire Mining and Metallurgical Congress, Australia and New Zealand (ed. Edwards, AB), pp. 284–96. Melbourne: Australasian Institute of Mining and Metallurgy.Google Scholar
Patiño-Douce, AE (1996) Effects of pressure and H2O content on the compositions of primary crustal melts. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 11–21.CrossRefGoogle Scholar
Patiño-Douce, AE and Beard, JS (1995) Dehydration-melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar. Journal of Petrology 36, 707–38.CrossRefGoogle Scholar
Patiño-Douce, AE and Harris, NBW (1998) Experimental constraints on Himalayan anatexis. Journal of Petrology 39, 689–710.CrossRefGoogle Scholar
Patiño-Douce, AE and Johnson, AD (1991) Phase equilibria and melt productivity in the pelitic system: implication for the origin of peraluminous granitoids and aluminous granulites. Contributions to Mineralogy and Petrology 107, 202–18.CrossRefGoogle Scholar
Patiño-Douce, AE and McCarthy, TC (1998) Melting of crustal rocks during continental collision and subduction. In When Continents Collide: Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks (eds Hacker, BR and Liou, JG), pp. 27–55. Dordrecht: Kluwer.CrossRefGoogle Scholar
Pattison, DRM and Harte, B (1988) Evolution of structurally contrasting anatectic migmatites in the 3-kbar Ballachulish aureole, Scotland. Journal of Metamorphic Geology 6, 475–94.CrossRefGoogle Scholar
Pichavant, M (1981) An experimental study of the effect of boron on a water saturated haplogranite at 1 kbar vapour pressure. Contributions to Mineralogy and Petrology 76, 430–9.CrossRefGoogle Scholar
Powell, R (1983) Processes in granulite-facies metamorphism. In Migmatites, Melting and Metamorphism (eds Atherton, MP and Gribble, CD), pp. 127–39. Nantwich, Cheshire: Shiva.Google Scholar
Powell, R, Holland, TJB and Worley, B (1998) Calculating phase diagram involving solid solutions via no-linear equations, with examples using THERMOCALC. Journal of Metamorphic Geology 16, 577–86.CrossRefGoogle Scholar
Puziewicz, J and Johannes, W (1988) Phase equilibria and compositions of Fe–Mg–Al minerals and melts in water-saturated peraluminous granitic systems. Contributions to Mineralogy and Petrology 100, 156–68.CrossRefGoogle Scholar
Rabinowicz, M and Vigneresse, JÄ (2004) Melt segregation under compaction and shear channeling: application to granitic magma segregation in a continental crust. Journal of Geophysical Research: Solid Earth 109, 1978–2012.CrossRefGoogle Scholar
Redler, C,White, RW and Johnson, TE (2013) Migmatites in the Ivrea Zone (NW Italy): constraints on partial melting and melt loss in metasedimentary rocks from Val Strona di Omegna. Lithos 175–176, 40–53.CrossRefGoogle Scholar
Reichardt, H and Weinberg, RF (2012) Hornblende chemistry in meta- and diatexites and its retention in the source of leucogranites: an example from the Karakoram Shear Zone, NW India. Journal of Petrology 53, 1287–318.CrossRefGoogle Scholar
Rigby, MJ, Droop, GTR and Bromiley, GD (2008) Variations in fluid activity across the Etive thermal aureole, Scotland: evidence from cordierite volatile contents. Journal of Metamorphic Geology 26, 331–46.CrossRefGoogle Scholar
Rosenberg, CL and Handy, MR (2005) Experimental deformation of partially melted granite revisited: implications for the continental crust. Journal of Metamorphic Geology 23, 19–28.CrossRefGoogle Scholar
Rosenberg, CL and Riller, U (2000) Partial melt topology in statically and dynamically recrystallised granite. Geology 28, 7–10.2.0.CO;2>CrossRefGoogle Scholar
Rubatto, D, Hermann, J and Buick, IS (2006) Temperature and bulk composition control on the growth of monazite and zircon during low-pressure anatexis (Mount Stafford, central Australia). Journal of Petrology 47, 1973–96.CrossRefGoogle Scholar
Sawyer, EW (2010) Migmatites formed by water-fluxed partial melting of a leucogranodiorite protolith: microstructures in the residual rocks and source of the fluid. Lithos 116, 273–86.CrossRefGoogle Scholar
Scrimgeour, I, Smith, JB and Raith, JG (2001) Palaeoproterozoic high-T, low-P metamorphism and dehydration melting in metapelites from the Mopunga Range, Arunta Inlier, central Australia. Journal of Metamorphic Geology 19, 739–57.CrossRefGoogle Scholar
Skjerlie, KP and Johnston, AD (1992) Vapor-absent melting at 10 kbar of a biotite- and amphibole-bearing tonalitic gneiss: implications for the generation of A-type granites. Geology 20, 263–6.2.3.CO;2>CrossRefGoogle Scholar
Skjerlie, KP, Patiño-Douce, AE and Johnston, AD (1993) Fluid absent melting of a layered crustal protolith: implications for the generation of anatectic granites. Contributions to Mineralogy and Petrology 114, 365–78.CrossRefGoogle Scholar
Slagstad, T, Jamieson, RA and Culshaw, NG (2005) Formation, crystallization, and migration of melt in the mid-orogenic crust: Muskoka domain migmatites, Grenville Province, Ontario. Journal of Petrology 46, 893–919.CrossRefGoogle Scholar
Solar, GS and Brown, M (2001) Petrogenesis of migmatites in Maine, USA. Possible source of peraluminous granite in plutons. Journal of Petrology 42, 789–823.CrossRefGoogle Scholar
Stevens, G, Clemens, JD and Droop, GTR (1997) Melt production during granulite-facies anatexis: experimental data from “primitive” metasedimentary protoliths. Contributions to Mineralogy and Petrology 128, 352–70.CrossRefGoogle Scholar
Stewart, AJ (1981) Reynolds Range Region, Northern Territory, 1:100 000 Geological Map Commentary. Canberra, ACT: Bureau of Mineral Resources, Geology and Geophysics, 22 pp.Google Scholar
Stewart, AJ, Shaw, RD and Black, LP (1984) The Arunta Inlier: a complex ensialic mobile belt in central Australia. Part 1: stratigraphy, correlations and origin. Australian Journal of Earth Sciences 31, 445–55.CrossRefGoogle Scholar
Stuart, CA, Daczko, NR and Piazolo, S (2017) Local partial melting of the lower crust triggered by hydration through melt–rock interaction: an example from Fiordland, New Zealand. Journal of Metamorphic Geology 35, 213–30.CrossRefGoogle Scholar
Stuart, CA, Piazolo, S and Daczko, NR (2016) Mass transfer in the lower crust: evidence for incipient melt assisted flow along grain boundaries in the deep arc granulites of Fiordland, New Zealand. Geochemistry, Geophysics, Geosystems 17, 3733–53.CrossRefGoogle Scholar
Thompson, AB (1982) Dehydration melting of pelitic rocks and the generation of H2O-undersaturated granitic liquids. American Journal of Science 282, 1567–95.CrossRefGoogle Scholar
Thompson, AB and Connolly, JAD (1995) Melting of the continental crust: some thermal and petrological constraints on anatexis in continental collision zones and other tectonic settings. Journal of Geophysical Research 100, 15565–79.CrossRefGoogle Scholar
Tuttle, OF and Bowen, NL (1958) Origin of Granite in the Light of Experimental Studies in the System NaA1Si3O8–KA1Si3O8–SiO2–H2O. Geological Society of America Memoir no. 74.Google Scholar
Vernon, RH, Clarke, GL and Collins, WJ (1990) Local, mid-crustal granulite facies metamorphism and melting: an example in the Mount Stafford area, central Australia. In High Temperature Metamorphism and Crustal Anatexis (eds Ashworth, JR and Brown, M), pp. 272–319. London: Unwin Hyman.CrossRefGoogle Scholar
Vielzeuf, D and Holloway, JR (1988) Experimental determination of the fluid-absent melting relations in the pelitic system. Contributions to Mineralogy and Petrology 98, 257–76.CrossRefGoogle Scholar
Vielzeuf, D and Montel, JM (1994) Partial melting of metagreywackes. Part I. Fluid-absent experiments and phase relationships. Contributions to Mineralogy and Petrology 117, 375–93.CrossRefGoogle Scholar
Vry, J, Compston, W and Cartwright, I (1996) SHRIMP II dating of zircons and monazites: reassessing the timing of high-grade metamorphism and fluid flow in the Reynolds Range, northern Arunta Block, Australia. Journal of Metamorphic Geology 14, 335–50.CrossRefGoogle Scholar
Walte, NP, Bons, PD and Passchier, CW (2005) Deformation of melt-bearing systems – insight from in situ grain-scale analogue experiments. Journal of Structural Geology 27, 1666–79.CrossRefGoogle Scholar
Wang, W, Dunkley, E, Clarke, GL and Daczko, NR (2014a) The evolution of zircon during low-P partial melting of metapelitic rocks: theoretical predictions and a case study from Mt Stafford, central Australia. Journal of Metamorphic Geology 32, 791–808.CrossRefGoogle Scholar
Wang, W, Liu, XS, Hu, JM, Li, ZH, Zhao, Y, Zhai, MG, Liu, XC, Clarke, GL, Zhang, SH and Qu, HJ (2014b) Late Paleoproterozoic medium-P high grade metamorphism of basement rocks beneath the northern margin of the Ordos Basin, NW China: petrology, phase equilibrium modelling and U–Pb geochronology. Precambrian Research 251, 181–96.CrossRefGoogle Scholar
Ward, R, Stevens, G and Kisters, A (2008) Fluid and deformation induced partial melting and melt volumes in low-temperature granulite-facies metasediments, Damara Belt, Namibia. Lithos 105, 253–71.CrossRefGoogle Scholar
Warren, RG (1983) Metamorphic and tectonic evolution of granulites, Arunta Block, central Australia. Nature 305, 300–3.CrossRefGoogle Scholar
Weinberg, RF and Hasalová, P (2015) Water-fluxed melting of the continental crust: a review. Lithos 212–215, 158–88.CrossRefGoogle Scholar
Wells, PRA (1981) Accretion of continental crust: thermal and geochemical consequences. Philosophical Transactions of the Royal Society of London, Series A 301, 347–57.CrossRefGoogle Scholar
White, AJR, Chappell, BW and Cleaty, JR (1974) Geologic setting and emplacement of some Australian Paleozoic batholiths and implications for intrusion mechanisms. Pacific Geology 8, 159–71.Google Scholar
White, RW, Pomroy, NE and Powell, R (2005) An in-situ metatexite-diatexite transition in upper amphibolite facies rocks from Broken Hill, Australia. Journal of Metamorphic Geology 23, 579–602.CrossRefGoogle Scholar
White, RW and Powell, R (2002) Melt loss and the preservation of granulite facies mineral assemblages. Journal of Metamorphic Geology 20, 621–32.Google Scholar
White, RW, Powell, R and Clarke, GL (2002) The interpretation of reaction textures in Fe-rich metapelitic granulites of the Musgrave Block, central Australia: constraints from mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3– SiO2–H2O–TiO2–Fe2O3. Journal of Metamorphic Geology 20, 41–55.CrossRefGoogle Scholar
White, RW, Powell, R and Clarke, GL (2003) Prograde metamorphic assemblage evolution during partial melting of metasedimentary rocks at low pressures: migmatites from Mt Stafford, central Australia. Journal of Petrology 44, 1931–60.CrossRefGoogle Scholar
White, RW, Powell, R and Holland, TJW (2001) Calculation of partial melting equilibria in the system Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O (NCKFMASH). Journal of Metamorphic Geology 19, 139–53.CrossRefGoogle Scholar
White, RW, Powell, R and Holland, TJB (2007) Progress relating to calculation of partial melting equilibria for metapelites. Journal of Metamorphic Geology 25, 511–27.CrossRefGoogle Scholar
White, RW, Powell, R, Holland, TJB and Worley, BA (2000) The effect of TiO2 and Fe2O3 on metapelitic assemblages at greenschist and amphibolite facies conditions: mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–Fe2O3. Journal of Metamorphic Geology 18, 497–511.CrossRefGoogle Scholar
White, RW, Stevens, G and Johnson, TE (2011) Is the crucible reproducible? Reconciling melting experiments with thermodynamic calculations. Elements 7, 241–6.CrossRefGoogle Scholar
Wickham, SM (1987) Crustal anatexis and granite petrogenesis during low-pressure regional metamorphism–the Trois Seigneurs Massif, Pyrenees, France. Journal of Petrology 28, 127–69.CrossRefGoogle Scholar
Yakymchuk, C and Brown, M (2014) Consequences of open-system melting in tectonics. Journal of the Geological Society, London 171, 21–40.CrossRefGoogle Scholar
Yardley, BWD (2009) The role of water in the evolution of the continental crust. Journal of the Geological Society, London 166, 585–600.CrossRefGoogle Scholar
Yardley, BWD and Barber, JP (1991) Melting reactions in the Connemara schists – the role of water infiltration in the formation of amphibolite facies migmatites. American Mineralogist 76, 848–56.Google Scholar
Yardley, BWD and Valley, JW (1997) The petrologic case for a dry lower crust. Journal of Geophysical Research 102, 12173–85.CrossRefGoogle Scholar
Yardley, BWD and Valley, JW (2000) Comment on “The petrologic case for a dry lower crust” by Yardley, B. W. D. & Valley, J. W. – Reply. Journal of Geophysical Research 105, 6065–8.CrossRefGoogle Scholar
Supplementary material: File

Wang et al. supplementary material

Wang et al. supplementary material 1

Download Wang et al. supplementary material(File)
File 23 KB
Supplementary material: File

Wang et al. supplementary material

Wang et al. supplementary material 2

Download Wang et al. supplementary material(File)
File 14.3 KB
Supplementary material: File

Wang et al. supplementary material

Wang et al. supplementary material 3

Download Wang et al. supplementary material(File)
File 14.4 KB