Abstract
Plate subduction is the most magnificent process in the Earth. Subduction zones are important sites for proceeding matter- and energy- transports between the Earth’s surface and the interior, continental crust growth, and crust-mantle interactions. Besides, a number of geological processes in subduction zones are closely related to human beings’ daily life, such as volcanic eruptions and earthquakes, formation of mineral deposits. Subduction process thus has long been the centric topic of Earth sciences. The finding in 1980s that continental crust could be subducted to mantle depths is a revolutionary progress in plate tectonic theory. Compared to oceanic crust, continental crust is colder, drier, lighter, and much more geochemically/isotopically heterogeneous Hence, continental subduction process would affect the structure, compositions and evolutions of the overlying mantle wedge even more. During continental subduction and subsequent exhumation, fluids and melts can be generated in the (de)hydration process and partial melting process, respectively. These melts/fluids play important roles in crust-mantle interactions, elemental migrations, isotopic fractionations, and mantle metasomatism. By summarizing recent research works on subduction zones in this paper, we present a review on the types, physicochemical conditions and compositions of fluids/melts, as well as the migration behaviors of fluid-related characteristic elements (Nb-Ta-V) and the fractionation behaviors of non-traditional stable isotopes (Li-Mg) in subduction zones. The aim of this paper is to provide the readers an update comprehensive overview of the melt/fluid activities in subduction zones and of Li-Mg isotope systematics in subduction-related rocks and minerals.
Similar content being viewed by others
References
Abers G A, Nakajima J, van Keken P E, Kita S, Hacker B R. 2013. Thermal-petrological controls on the location of earthquakes within subducting plates. Earth Planet Sci Lett, 369: 178–187
Agostini S, Ryan J G, Tonarini S, Innocenti F. 2008. Drying and dying of a subducted slab: Coupled Li and B isotope variations in Western Anatolia Cenozoic Volcanism. Earth Planet Sci Lett, 272: 139–147
Ague J J, Nicolescu S. 2014. Carbon dioxide released from subduction zones by fluid-mediated reactions. Nat Geosci, 7: 355–360
Alt J, Burdett J. 1992. Sulfur in Pacific deep-sea sediments (Leg 129) and implications for cycling of sediment in subduction zones. Proc ODP Sci Res. 283–294
Alt J C. 1995. Sulfur isotopic profile through the oceanic crust: Sulfur mobility and seawater-crustal sulfur exchange during hydrothermal alteration. Geology, 23: 585–588
Alt J C, Anderson T F, Bonnell L. 1989. The geochemistry of sulfur in a 1.3 km section of hydrothermally altered oceanic crust, DSDP Hole 504B. Geochim Cosmochim Acta, 53: 1011–1023
Alt J C, Garrido C J, Shanks W, Turchyn A, Padrón-Navarta J A, Sánchez-Vizcaíno V L, Pugnaire M T G, Marchesi C. 2012. Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain. Earth Planet Sci Lett, 327: 50–60
Alt J C, Shanks W C. 2011. Microbial sulfate reduction and the sulfur budget for a complete section of altered oceanic basalts, IODP Hole 1256. (eastern Pacific). Earth Planet Sci Lett, 310: 73–83
Antignano A, Manning C E. 2008. Rutile solubility in H2O, H2O-SiO2, and H2O-NaAlSi3O8 uids at 0.7–2.0 GPa and 700–1000°C: Implications for mobility of nominally insoluble elements. Chem Geol, 255: 283–293
Auzanneau E, Vielzeuf D, Schmidt M. 2006. Experimental evidence of decompression melting during exhumation of subducted continental crust. Contrib Mineral Petrol, 152: 125–148
Barth M, McDonough W F, Rudnick R L. 2000. Tracking the budget of Nb and Ta in the continental crust. Chem Geol 165: 197–213
Beaumont C, Jamieson R A, Butler J P, Warren C J. 2009. Crustal structure: A key constraint on the mechanism of ultra-high-pressure rock exhumation. Earth Planet Sci Lett, 287: 116–129
Bebout G E. 2007. Metamorphic chemical geodynamics of subduction zones. Earth Planet Sci Lett, 260: 373–393
Bebout G E, Marilyn L F, Cartigny P. 2013a. Nitrogen: Highly volatile yet surprisingly compatible. Elements, 9: 333–338
Bebout G E, Agard P, Kobayashi K, Moriguti T, Nakamura E. 2013b. Devolatilization history and trace element mobility in deeply subducted sedimentary rocks: Evidence from Western Alps HP/UHP suites. Chem Geol, 342: 1–20
Behn M D, Kelemen P B, Hirth G, Hacker B R, Massonne H J. 2011. Diapirs as the source of the sediment signature in arc lavas. Nat Geosci, 4: 641–646
Beinlich A, Klemd R, John T, Gao J. 2010. Trace-element mobilization during Ca-metasomatism along a major fluid conduit: Eclogitization of blueschist as a consequence of fluid-rock interaction. Geochim Cosmochim Acta, 74: 1892–1922
Berkesi M, Guzmics T, Szabó C, Dubessy J, Bodnar R J, Hidas K, Ratter K. 2012. The role of CO2-rich fluids in trace element transport and metasomatism in the lithospheric mantle beneath the Central Pannonian Basin, Hungary, based on fluid inclusions in mantle xenoliths. Earth Planet Sci Lett, 331: 8–20
Blundy J, Cashman K, Humphreys M. 2006. Magma heating by decompression-driven crystallization beneath and esite volcanoes. Nature, 443: 76–80
Blundy J, Wood B. 2003. Partitioning of trace elements between crystals and melts. Earth Planet Sci Lett, 210: 383–397
Bourdon B, Tipper E T, Fitoussi C, Stracke A. 2010. Chondritic Mg isotope composition of the Earth. Geochim Cosmochim Acta, 74: 5069–5083
Bromiley G D, Pawley A R. 2003. The stability of antigorite in the systems MgO-SiO2-H2O (MSH) and MgO-Al2O3-SiO2-H2O (MASH): The effects of Al3+ substitution on high-pressure stability. Am Mineral, 88: 99–108
Brovarone V A, Alard O, Beyssac O, Martin L, Picatto M. 2014. Lawsonite metasomatism and trace element recycling in subduction zones. J Metamorph Geol, 32: 489–514
Burton M R, Sawyer G M, Granieri D. 2013. Deep carbon emissions from volcanoes. Rev Mineral Geochem, 75: 323–354
Caciagli N, Brenan J, McDonough W F, Phinney D. 2011. Mineral-fluid partitioning of lithium and implications for slab-mantle interaction. Chem Geol, 280: 384–398
Canfield D E. 2004. The evolution of the Earth surface sulfur reservoir. Am J Sci, 304: 839–861
Carmichael I. 2002. The andesite aqueduct: Perspectives on the evolution of intermediate magmatism in west-central (105°–99°W) Mexico. Contrib Mineral Petrol, 143: 641–663
Cartigny P, Marty B. 2013. Nitrogen isotopes and mantle geodynamics: The emergence of life and the Atmosphere-Crust-Mantle connection. Elements, 9: 359–364
Cervantes P, Wallace P. 2003. Magma degassing and basaltic eruption styles: A case study of ~2000 year BP Xitle volcano in central Mexico. J Volcanol Geotherm Res, 120: 249–270
Chen R X, Zheng Y F, Gong B. 2011. Mineral hydrogen isotopes and water contents in ultrahigh-pressure metabasite and metagranite: Constraints on fluid flow during continental subduction-zone metamorphism. Chem Geol, 281: 103–124
Chen Y X, Zheng Y F, Hu Z. 2013a. Petrological and zircon evidence for anatexis of UHP quartzite during continental collision in the Sulu orogen. J Metamorph Geol, 31: 389–413
Chen Y, Ye K, Wu Y W, Guo S, Su B, Liu J B. 2013b. Hydration and dehydration in the lower margin of a cold mantle wedge: Implications for crust-mantle interactions and petrogeneses of arc magmas. Int Geol Rev, 55: 1506–1522
Chen Y, Ye K, Su B, Guo S, Liu J B. 2013c. Metamorphism and metasomatism of orogenic peridotites from Dabie-Sulu UHP terrane (in Chinese). Chin Sci Bull, 58: 2294–2299
Chopin C. 1984. Coesite and pure pyrope in high-grade blueschists of the Western Alps: A first record and some consequences. Contrib Mineral Petrol, 86: 107–118
Clarke G, Powell R, Fitzherbert J. 2006. The lawsonite paradox: A comparison of field evidence and mineral equilibria modelling. J Metamorph Geol, 24: 715–725
Cloos M, Shreve R L. 1988a. Subduction-channel model of prism accretion, mélange formation, sediment subduction, and subduction erosion atconvergent plate margins: 1, Background and description. Pure Appl Geophys, 128: 455–500
Cloos M, Shreve R L. 1988b. Subduction-channel model of prism accretion, mélange formation, sediment subduction, and subduction erosion at convergent plate margins: 2, Implications and discussion. Pure Appl Geophys, 128: 501–505
Connolly J. 2005. Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation. Earth Planet Sci Lett, 236: 524–541
Cooper L B, Ruscitto D M, Plank T, Wallace P J, Syracuse E M, Manning C E. 2012. Global variations in H2O/Ce: 1. Slab surface temperatures beneath volcanic arcs. Geochem Geophys Geosyst, 13, doi: 10.1029/ 2011GC003902
Cottrell E, Kelley K A. 2011. The oxidation state of Fe in MORB glasses and the oxygen fugacity of the upper mantle. Earth Planet Sci Lett, 305: 270–282
Crerar D, Wood S, Brantley S, Bocarsly A. 1985. Chemical controls on solubility of ore-forming minerals in hydrothermal solutions. Can Mineral, 23: 333–352
Davies J H, Stevenson D J. 1992. Physical model of source region of subduction zone volcanics. J Geophys Res, 97: 2037–2070
Defant M J, Drummond M S. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347: 662–665
Deschamps F, Godard M, Guillot S, Hattori K. 2013. Geochemistry of subduction zone serpentinites: A review. Lithos, 178: 96–127
Dobrzhinetskaya L F, Green II H W, Wang S. 1996. Alpe Arami: A pridotite massif from depths of more than 300 kilometers. Science, 271: 1841–1845
Dohmen R, Kasemann S A, Coogan L, Chakraborty S. 2010. Diffusion of Li in olivine. Part I: Experimental observations and a multi species diffusion model. Geochim Cosmochim Acta, 74: 274–292
Dvir O, Pettke T, Fumagalli P, Kessel R. 2011. Fluids in the peridotite-water system up to 6 GPa and 800°C: New experimental constrains on dehydration reactions. Contrib Mineral Petrol, 161: 829–844
Eggler D H, Burnham C W. 1984. Solution of H2O in diopside melts— a thermodynamic model. Contrib Mineral Petrol, 85: 58–66
Enami M, Liou J G, Mattinson C G. 2004. Epidote minerals in high P/T metamorphic terranes: Subduction zone and high- to ultrhigh-pressure metamorphism. Rev Mineral Geochem, 56: 347–398
Ernst W, Tsujimori T, Zhang R, Liou J G. 2007. Permo-Triassic collision, subduction-zone metamorphism, and tectonic exhumation along the East Asian continental margin. Annu Rev Earth Planet Sci, 35: 73–110
Ferrando S, Frezzotti M, Dallai L, Compagnoni R. 2005. Multiphase solid inclusions in UHP rocks (Su-Lu, China): Remnants of supercritical silicate-rich aqueous fluids released during continental subduction. Chem Geol, 223, 68–81
Foley S F, Barth M G, Jenner G A. 2000. Rutile/melt partition coefficients for trace elements and an assessment of the influence of rutile on the trace element characteristics of subduction zone magmas. Geochim Cosmochim Acta, 64: 933–938
Foley S, Tiepolo M, Vannucci R. 2002. Growth of early continental crust controlled by melting of amphibolite in subduction zones. Nature, 417: 837–840
Frezzotti M, Selverstone J, Sharp Z, Compagnoni R. 2011. Carbonate dissolution during subduction revealed by diamond-bearing rocks from the Alps. Nat Geosci, 4: 703–706
Frezzotti M L, Ferrando S, Tecce F, Castelli D. 2012. Water content and nature of solutes in shallow-mantle fluids from fluid inclusions. Earth Planet Sci Lett, 351: 70–83
Fu B, Touret J L R, Zheng Y F. 2001. Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe, Dabie Shan (China). J Metamorph Geol, 19: 531–547
Fu B, Touret J L, Zheng Y F, Jahn B M. 2003. Fluid inclusions in granulites, granulitized eclogites and garnet clinopyroxenites from the Dabie-Sulu terranes, eastern China. Lithos, 70: 293–319
Fumagalli P, Poli S. 2005. Experimentally determined phase relations in hydrous peridotites to 6.5 GPa and their consequences on the dynamics of subduction zones. J Petrol, 46: 555–578
Fumagalli P, Zanchetta S, Poli S. 2009. Alkali in phlogopite and amphibole and their effects on phase relations in metasomatized peridotites: A high-pressure study. Contrib Mineral Petrol, 158: 723–737
Gaetani G A, Grove T L. 1998. The influence of water on melting of mantle peridotite. Contrib Mineral Petrol, 131: 323–346
Gaetani G A, Grove T L. 2003. Experimental constraints on melt generation in the mantle wedge. In: Eiler J ed. Inside the Subduction Factory. Washington D C: AGU Geophysical Monograph Series. 107–134
Gao J, John T, Klemd R, Xiong X M. 2007. Mobilization of Ti-Nb-Ta during subduction: Evidence from rutile–bearing dehydration segregations and veins hosted in eclogite, Tianshan, NW China. Geochim Cosmochim Acta, 71: 4974–4996
Gao X Y, Zheng Y F, Chen Y X. 2012. Dehydration melting of ultrahigh-pressure eclogite in the Dabie orogen: Evidence from multiphase solid inclusions in garnet. J Metamorph Geol, 30: 193–212
Gao X Y, Zheng Y F, Chen Y X, Hu Z. 2013. Trace element composition of continentally subducted slab-derived melt: Insight from multiphase solid inclusions in ultrahigh-pressure eclogite in the Dabie orogen. J Metamorph Geol, 31: 453–468
Gill J B. 1981. Geophysical Setting of Volcanism at Convergent Plate Boundaries, Orogenic Andesites and Plate Tectonics. Berlin: Springer. 44–63
Goldblatt C, Claire M W, Lenton T M, Matthews A J, Watson A J, Zahnle K J. 2009. Nitrogen-enhanced greenhouse warming on early Earth. Nat Geosci, 2: 891–896
Green D H, Hibberson W O, Kovács I, Rosenthal A. 2010. Water and its influence on the lithosphere-asthenosphere boundary. Nature, 467: 448–451
Grove T L, Chatterjee N, Parman S W, Médard E. 2006. The influence of H2O on mantle wedge melting. Earth Planet Sci Lett, 249: 74–89
Grove T L, Elkins-Tanton L T, Parman S W, Chatterjee N, Müntener O, Gaetani G A. 2003. Fractional crystallization and mantle-melting controls on calc-alkaline differentiation trends. Contrib Mineral Petrol, 145: 515–533
Grove T L, Till C B, Krawczynski M. 2012. The role of H2O in subduction zone magmatism. Annu Rev Earth Planet Sci, 40: 413–439
Gorman P J, Kerrick D, Connolly J. 2006. Modeling open system metamorphic decarbonation of subducting slabs. Geochem Geophys Geosyst, 7, doi: 10.1029/2005GC001125
Guillot S, Hattori K, Agard P, Schwartz S, Vidal O. 2009. Exhumation processes in oceanic and continental subduction contexts: A review. In: Lallemand S, Funiciello F, eds. Subduction Zone Geodynamics. Berlin: Springer-Verlag. 175–205
Guo S, Ye K, Chen Y, Liu J B, Mao Q, Ma Y G. 2012. Fluid-rock interaction and element mobilization in UHP metabasalt: Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen. Lithos, 136: 145–167
Hack A C, Thompson A B. 2011. Density and viscosity of hydrous magmas and related fluids and their role in subduction zone processes. J Petrol, 52:1333–1362
Hacker B R. 2008. H2O subduction beyond arcs. Geochem Geophs Geosyst, 9, doi: 10.1029/2007GC001707
Hauri E H, Wagner T P, Grove T L. 1994. Experimental and natural partitioning of Th, U, Pb and other trace-elements between garnet, clinopyroxene and basaltic melts. Chem Geol, 117: 149–166
Hermann J, Martin L. 2012. CO2 analysis in high-pressure melts and implications for carbon recycling in subduction zones. EGU General Assembly Conference Abstracts. 3800
Hermann J, Rubatto D. 2009. Accessory phase control on the trace element signature of sediment melts in subduction zones. Chem Geol, 265: 512–526
Hermann J, Rubatto D. 2014. Subduction of continental crust to mantle depth: Geochemistry of ultrahigh-pressure rocks. In: Holland H D, Turekian K K, eds. Treatise on Geochemistry. 2nd ed. Vol 4. 309–340
Hermann J, Spandler C J. 2008. Sediment melts at sub-arc depths: An experimental study. J Petrol, 49: 717–740
Hermann J, Rubatto D, Korsakov A, Shatsky V S. 2001. Multiple zircon growth during fast exhumation of diamondiferous, deeply subducted continental crust (Kokchetav Massif, Kazakhstan). Contrib Mineral Petrol, 141: 66–82
Hermann J, Spandler C, Hack A, Korsakov A V. 2006. Aqueous fluids and hydrous melts in high-pressure and ultra-high pressure rocks: Implications for element transfer in subduction zones. Lithos, 92: 399–417
Hermann J, Zheng Y F, Rubatto D. 2013. Deep fluids in subducted continental crust. Elements, 9: 281–287
Hirose K. 1997. Partial melt compositions of carbonated peridotite at 3 GPa and role of CO2 in alkali-basalt magma generation. Geophys Res Lett, 24: 2837–2840.
Hirose K, Kawamoto T. 1995. Hydrous partial melting of iherzolite at 1 GPa-the effect of H2O on the genesis of basaltic magmas. Earth Planet Sci Lett, 133: 463–473
Honma H, Itihara Y. 1981. Distribution of ammonium in minerals of metamorphic and granitic rocks. Geochim Cosmochim Acta, 45: 983–988
Huang F, Chen L J, Wu Z Q, Wang W. 2013. First-principles calculations of equilibrium Mg isotope fractionations between garnet, clinopyroxene, orthopyroxene, and olivine: Implications for Mg isotope thermometry. Earth Planet Sci Lett, 367: 61–70
Huang J, Xiao Y L, Gao Y J, Hou Z H, Wu W P. 2012a. Nb-Ta fractionation induced by fluid-rock interaction in subduction-zones: Constraints from UHP eclogites- and vein-hosted rutile from the Dabie orogen, Central-Eastern China. J Metamorph Geol, 30: 821–842
Huang J, Xiao Y L. 2015. Element mobility in mafic and felsic ultrahigh pressure metamorphic rocks from the South Dabie orogen, China: Insights into supercritical fluids in continental subduction zones. Int Geol Rev, 57: 1103–1129
Jarrard R D. 2003. Subduction fluxes of water, carbon dioxide, chlori ne, and potassium. Geochem Geophs Geosyst, 4, doi: 10.1029/200 2GC000392
Jégo S, Dasgupta R. 2013. Fluid-present melting of sulfide-bearing ocean-crust: Experimental constraints on the transport of sulfur from subducting slab to mantle wedge. Geochim Cosmochim Acta, 110: 106–134
Jégo S, Dasgupta R. 2014. The fate of sulfur during fluid-present melting of subducting basaltic crust at variable oxygen fugacity. J Petrol, 55: 1019–1050
Jahn S, Wunder B. 2009. Lithium speciation in aqueous fluids at high P and T studied by ab initio molecular dynamics and consequences for Li-isotope fractionation between minerals and fluids. Geochim Cosmochim Acta, 73: 5428–5434
John T, Klemd R, Gao J, Garbe-Schönberg C D. 2008. Trace-element mobilization in slabs due to non steady-state fluid-rock interaction: Constraints from an eclogites-facies transport vein in blueschist (Tianshan, China). Lithos, 103: 1–24
John T, Schenk V. 2006. Interrelations between intermediate-depth earthquakes and fluid flow within subducting oceanic plates: Constraints from eclogite facies pseudotachylytes. Geology, 34: 557–560
Kawamoto T, Kanzaki M, Mibe K, Matsukage K N, Ono S. 2012. Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism. Proc Natl Acad Sci USA, 109: 18695–18700
Kawamoto T, Yoshikawa M, Kumagai Y, Mirabueno M H, Okuno M, Kobayashi T. 2013. Mantle wedge infiltrated with saline fluids from dehydration and decarbonation of subducting slab. Proc Natl Acad Sci USA, 110: 9663–9668
Kelemen P B, Rilling J L, Parmentier E, Mehl L, Hacker B R. 2003. Thermal structure due to solid-state flow in the mantle wedge beneath arcs. Inside the subduction factory. 293–311
Kelley K A, Plank T, Ludden J, Staudigel H. 2003. Composition of altered oceanic crust at ODP Sites 801 and 1149. Geochem Geophs Geosyst, 4, doi: 10.1029/2002GC000435
Kennedy G, Wasserburg G, Heard H, Newton R. 1962. The upper three phase region in the system SiO2-H2O. Am J Sci, 260: 501–521
Kerrick D, Connolly J. 2001. Metamorphic devolatilization of subducted oceanic metabasalts: Implications for seismicity, arc magmatism and volatile recycling. Earth Planet Sci Lett, 189: 19–29
Kessel R, Schmidt M W, Ulmer P, Pettke T. 2005a. Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth. Nature, 437: 724–727
Kessel R, Ulmer P, Pettke T, Schmidt M, Thompson A. 2005b. The water-basalt system at 4 to 6 GPa: Phase relations and second critical endpoint in a K-free eclogite at 700 to 1400°C. Earth Planet Sci Lett, 237: 873–892
Klemme S, Prowatke S, Hametner K, Günther D. 2005. Partitioning of trace elements between rutile and silicate melts: Implications for subduction zones. Geochim Cosmochim Acta, 69: 2361–2371
Klimm K, Blundy J D, Green T H. 2008. Trace element partitioning and accessory phase saturation during H2O-saturated melting of basalt with implications for subduction zone chemical fluxes. J Petrol, 49: 523–553
Krawczynski. 2011. Experimental studies of melting and crystallization processes in planetary interiors. Doctoral Dissertation. Massachusetts Institute of Technology. 202
Krawczynski M J, Grove T L, Behrens H. 2012. Amphibole stability in primitive arc magmas: Effects of temperature, H2O content, and oxygen fugacity. Contrib Mineral Petrol, 164: 317–339
Kushiro K. 1990. Partial melting of mantle wedge and evolution of island arc crust. J Geophys Res, 95: 15929–15939
Labrousse L, Prouteau G, Ganzhorn A C. 2011. Continental exhumation triggered by partial melting at ultrahigh pressure. Geology, 39: 1171–1174
Li W Y, Teng F Z, Ke S, Rudnick R L, Gao S, Wu F Y, Chappell B W. 2010. Heterogeneous magnesium isotopic composition of the upper continental crust. Geochim Cosmochim Acta, 74: 6867–6884
Li W Y, Teng F Z, Xiao Y L, Huang J. 2011. High-temperature intermineral magnesium isotope fractionation in eclogite from the Dabie orogen, China. Earth Planet Sci Lett, 304: 224–230
Li W Y, Teng F Z, Xiao Y, Huang J. 2014. Limited magnesium isotope fractionation during metamorphic dehydration in metapelites from the Onawa contact aureole, Maine. Geochem Geophys Geosyst, 15: 408–415
Li X P, Zheng Y F, Wu Y B, Chen F, Gong B, Li Y L. 2004. Low-T eclogite in the Dabie terrane of China: Petrological and isotopic constraints on fluid activity and radiometric dating. Contrib Mineral Petrol, 148: 443–470
Liu F L, Robinson P T, Liu P H. 2012. Multiple partial melting events in the Sulu UHP terrane: zircon U-Pb dating of granitic leucosomes within amphibolite and gneiss. J Metamorph Geol, 30: 887–906
Liu L, Xiao Y L, Aulbach S, Li D Y, Hou Z H. 2014. Vanadium and niobium behavior in rutile as a function of oxygen fugacity: Evidence from natural samples. Contrib Mineral Petrol, 167: 1026
Liu X W, Jin Z M, Green H W. 2007. Clinoenstatite exsolution in diopsidic augite of Dabieshan: Garnet peridotite from depth of 300 km. Am Mineral, 92: 546–552
Liu Y C, Gu X F, Rolfo F, Chen Z Y. 2011. Ultrahigh-pressure metamorphism and multistage exhumation of eclogite of the Luotian dome, North Dabie Complex Zone (central China): Evidence from mineral inclusions and decompression textures. J Asian Earth Sci, 42: 607–617
López Sánchez-Vizcaíno V, Gómez-Pugnaire M T, Garrido C J, Padrón-Navarta J A, Mellini M. 2009. Breakdown mechanisms of titanclinohumite in antigorite serpentinite (Cerro del Almirez massif, S. Spain): A petrological and TEM study. Lithos, 107: 216–226
Malaspina N, Hermann J, Scambelluri M. 2009. Fluid/mineral interaction in UHP garnet peridotite. Lithos, 107: 38–52
Malaspina N, Hermann J, Scambelluri M, Compagnoni R. 2006. Multistage metasomatism in ultrahigh-pressure mafic rocks from the North Dabie Complex (China). Lithos, 90: 19–42
Malaspina N, Tumiati S. 2012. The role of C-O-H and oxygen fugacity in subduction-zone garnet peridotites. Eur J Mineral, 24: 607–618
Mallmann G, O’Neill H S C. 2009. The crystal/melt partitioning of V during mantle melting as a function of oxygen fugacity compared with some other Elements (Al, P, Ca, Sc, Ti, Cr, Fe, Ga, Y, Zr and Nb). J Petrol, 50: 1765–1794
Manning C E. 1994. The solubility of quartz in H2O in the lower crust and upper-mantle. Geochim Cosmochim Acta, 58: 4831–4839
Manning C E. 2004. The chemistry of subduction-zone fluids. Earth Planet Sci Lett, 223: 1–16
Manning C E, Shock E L, Sverjensky D. 2013. The chemistry of carbon in aqueous fluids at crustal and uppermantle conditions: Experimental and theoretical constraints. Rev Mineral Geochem, 75: 109–148
Marschall H R, Dohmen R, Ludwig T. 2013. Diffusion-induced fractionation of niobium and tantalum during continental crust formation. Earth Planet Sci Lett, 375: 361–371
Marschall H R, Schumacher J. 2012. Arc magmas sourced from melange diapirs in subduction zones. Nat Geosci, 5: 862–867
Marschall H R, von Strandmann P A P, Seitz H M, Elliott T, Niu Y L. 2007. The lithium isotopic composition of orogenic eclogites and deep subducted slabs. Earth Planet Sci Lett, 262: 563–580
Martin L, Hermann J, Gauthiez-Putallaz L, Whitney D, Vitale Brovarone A, Fornash K, Evans N. 2014. Lawsonite geochemistry and stability— Implication for trace element and water cycles in subduction zones. J Metamorph Geol, 32: 455–478
McCammon C. 2005. The paradox of mantle redox. Science, 308: 807–808
Médard E, Grove T L. 2006. Early hydrous melting and degassing of the Martian interior. J Geophys Re, 111, doi: 10.1029/2006JE002742
Mibe K, Chou I M, Bassett W. 2008. In situ Raman spectroscopic investigation of the structure of subduction-zone fluids. J Geophys Res, 113, doi: 10.1029/2007JB005179
Mibe K, Fujii T, Yasuda A. 2002. Composition of aqueous fluid coexisting with mantle minerals at high pressure and its bearing on the differentiation of the Earth’s mantle. Geochim Cosmochim Acta, 66: 2273–2285
Mibe K, Kawamoto T, Matsukage K N, Fei Y, Ono S. 2011. Slab melting versus slab dehydration in subduction-zone magmatism. Proc Natl Acad Sci USA, 108: 8177–8182
Münker C, Pfänder J A, Weyer S, Büchl A, Kleine T, Mezger K. 2003. Evolution of planetary cores and the earth-moon system from Nb/Ta systematics. Science 301, 84–87
Padrón-Navarta J A, Sánchez-Vizcaíno V L, Garrido C J, Gómez-Pugnaire M T. 2011. Metamorphic record of high-pressure dehydration of antigorite serpentinite to chlorite harzburgite in a subduction setting (Cerro del Almirez, Nevado-Filábride Complex, Southern Spain). J Petrol, 52: 2047–2078
Pfänder J A, Münker C, Stracke A, Mezger K. 2007. Nb/Ta and Zr/Hf in ocean island basalts—Implications for crust-mantle differentiation and the fate of Niobium. Earth Planet Sci Lett, 254: 158–172
Paillat O, Elphick S, Brown W. 1992. The solubility of water in NaAlSi3O8 melts—A reexamination of AB-H2O phase-relationships and critical-behavior at high-pressures. Contrib Mineral Petrol, 112: 490–500.
Pan D, Spanu L, Harrison B, Sverjensky D A, Galli G. 2013. Dielectric properties of water under extreme conditions and transport of carbonates in the deep Earth. Proc Natl Acad Sci USA, 110: 6646–6650
Parkinson I J, Arculus R J. 1999. The redox state of subduction zones: Insights from arc-peridotites. Chem Geol, 160: 409–423
Parman S W, Grove T L. 2004. Harzburgite melting with and without H2O: Experimental data and predictive modeling. J Geophys Res, 109, doi: 10.1029/2003JB002566
Pawley A. 2003. Chlorite stability in mantle peridotite: The reaction clinochlore+ enstatite=forsterite+pyrope+H2O. Contrib Mineral Petrol, 144: 449–456.
Peacock S M. 1990. Fluid Processes in Subduction Zones. Science, 248: 329–337
Plank T, Langmuir C H. 1998. The chemical composition of subducting sediment and its consequences for the crust and mantle. Chem Geol, 145: 325–394
Plank T, Cooper L B, Manning C E. 2009. Emerging geothermometers for estimating slab surface temperatures. Nat Geosci, 2: 611–615
Poli S, Franzolin E, Fumagalli P, Crottini A. 2009. The transport of carbon and hydrogen in subducted oceanic crust: An experimental study to 5 GPa. Earth Planet Sci Lett, 278: 350–360
Prouteau G, Scaillet B. 2013. Experimental constraints on sulphur behaviour in subduction zones: Implications for TTG and adakite production and the global sulphur cycle since the Archean. J Petrol, 54:183–213
Prouteau G, Scaillet B, Pichavant M, Maury R. 2001. Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust. Nature, 410: 197–200
Rapp R P, Watson E B. 1995. Dehydration melting of metabasalt at 8–32 kbar: Implications for continental growth and crust-mantle recycling. J Petrol, 36: 891–931
Rapp R P, Shimizu N, Norman M D. 2003. Growth of early continental crust by partial melting of eclogite. Nature, 425: 605–609
Richter F. 2003. Isotope fractionation by chemical diffusion between molten basalt and rhyolite. Geochim Cosmochim Acta, 67: 3905–3923
Richter F M, McKenzie D P. 1978. Simple plate models of mantle convection. J Geophys, 44: 441–471
Rudnick R L, Barth M, Horn I, McDonough W F. 2000. Rutile-bearing refractory eclogites: Missing link between continents and depleted mantle. Science, 287: 278–281
Saffer D M, Tobin H J. 2011. Hydrogeology and mechanics of subduction zone forearcs: Fluid flow and pore pressure. Annu Rev Earth Planet Sci, 39: 157–186
Scambelluri M, Piccardo G B, Philippot P, Robbiano A, Negretti L. 1997. High salinity fluid inclusions formed from recycled seawater in deeply subducted alpine serpentinite. Earth Planet Sci Lett, 148: 485–499
Schmidt M W, Poli S. 1998. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet Sci Lett, 163: 361–379
Schmidt M W, Vielzeuf D, Auzanneau E. 2004. Melting and dissolution of subducting crust at high pressures: The key role of white mica. Earth Planet Sci Lett, 228: 65–84
Sheng Y M, Xia Q K, Dallai L, Yang X Z, Hao Y T. 2007. H2O contents and D/H ratios of nominally anhydrous minerals from ultrahigh-pressure eclogites of the Dabie orogen, eastern China. Geochim Cosmochim Acta, 71: 2079–2103
Shreve R L, Cloos M. 1986. Dynamics of sediment subduction, mélange formation, and prism accretion. J Geophys Res, 91: 10229–10245
Simon A C, Ripley E M. 2011. The role of magmatic sulfur in the formation of ore deposits. Rev Mineral Geochem, 73: 513–578
Simons K K, Harlow G E, Brueckner H K, Goldstein S L, Sorensen S S, Hemming N G, Langmuir C H. 2010. Lithium isotopes in Guatemalan and Franciscan HP-LT rocks: Insights into the role of sediment-derived fluids during subduction. Geochim Cosmochim Acta, 74: 3621–3641
Sinogeikin S V, Schilling F R, Bass J D. 2000. Single crystal elasticity of lawsonite. Am Mineral, 85: 1834–1837
Sisson T W, Grove T L. 1993. Temperatures and H2O contents of low-MgO high-alumina basalts. Contrib Mineral Petrol, 113: 167–184
Sisson T W, Layne G D. 1993. H2O in basalt and basaltic andesite glass inclusions from 4 subduction-related volcanos. Earth Planet Sci Lett, 117: 619–635
Skora S, Blund J. 2010. High-pressure hydrous phase relations of radiolarian clay and implications for the involvement of subducted sediment in arc magmatism. J Petrol, 51: 2211–2243
Smith D C. 1984. Coesite in clinopyroxene in the Caledonides and its implications for geodynamics. Nature, 310: 641–644
Sobolev N V, Shatsky V S. 1990. Diamond inclusions in garnets from metamorphic rocks: A new environment for diamond formation. Nature, 343: 742–746
Spandler C, Pirard C. 2013. Element recycling from subducting slabs to arc crust: A review. Lithos, 170: 208–223
Spandler C, Hermann J. 2006. High-pressure veins in eclogite from New Caledonia and their significance for fluid migration in subduction zones. Lithos, 89: 135–153
Spandler C, Mavrogenes J, Hermann J. 2007. Experimental constraints on element mobility from subducted sediments using high-P synthetic fluid/ melt inclusions. Chem Geol, 239: 228–249
Spandler C, Pettke T, Rubatto D. 2011. Internal and external fluid sources for eclogite-facies veins in the Monviso Meta-ophiolite, Western Alps: Implications for fluid flow in subduction zones. J Petrol, 52: 1207–1236
Stalder R, Ulmer P, Thompson A, Günther D. 2001. High pressure fluids in the system MgO-SiO2-H2O under upper mantle conditions. Contrib Mineral Petrol, 140: 607–618
Sun H, Xiao Y L, Gao Y J, Lai J Q, Hou Z H, Wang Y Y. 2013. Fluid and melt inclusions in the Mesozoic Fangcheng basalt from North China Craton: Implications for magma evolution and fluid/melt-peridotite reaction. Contrib Mineral Petrol, 165: 885–901
Sutton S, Karner J, Papike J, Delaney J, Shearer C, Newville M, Eng P, Rivers M, Dyar M. 2005. Vanadium K edge XANES of synthetic and natural basaltic glasses and application to microscale oxygen barometry. Geochim Cosmochim Acta, 69: 2333–2348
Syracuse E M, van Keken P, Abers G A. 2010. The global range of subduction zone thermal models. Phys Earth Planet Inter, 183: 73–90
Tang Y J, Zhang H F, Deloule E, Su B X, Ying J F, Xiao Y, Hu Y. 2012. Slab-derived lithium isotopic signatures in mantle xenoliths from northeastern North China Craton. Lithos, 149: 79–90
Tatsumi Y, Eggins S. 1995. Subduction Zone Magmatism, 1. Cambridge: Blackwell Science
Tatsumi Y, Hamilton D, Nesbitt R. 1986. Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas: Evidence from high-pressure experiments and natural rocks. J Volcanol Geotherm Res, 29: 293–309
Teng F Z, Li W Y, Ke S, Marty B, Dauphas N, Huang S, Wu F Y, Pourmand A. 2010. Magnesium isotopic composition of the Earth and chondrites. Geochim Cosmochim Acta, 74: 4150–4166
Thorkelson D J, Breitsprecher K. 2005. Partial melting of slab window margins: Genesis of adakitic and non-adakitic magmas. Lithos, 79: 25–41
Tiepolo M, Vannucci R, Oberti R, Foley S, Bottazzi P, Zanetti A. 2000. Nb and Ta incorporation and fractionation in titanian pargasite and kaersutite: Crystal-chemical constraints and implications for natural systems. Earth Planet. Sci Lett, 176: 185–201
Till C B, Grove T L, Withers A C. 2012. The beginnings of hydrous mantle wedge melting. Contrib Mineral Petrol, 163: 669–688
Tomlinson E L, Mueller W, Eimf. 2009. Coexisting fluid (LA-ICP-MS) and silicate (SIMS) inclusions in fibrous diamonds. Earth Planet Sci Lett, 279: 362–372
Trommsdorff V, Sánchez-Vizcaíno V L, Gomez-Pugnaire M, Müntener O. 1998. High pressure breakdown of antigorite to spinifex-textured olivine and orthopyroxene, SE Spain. Contrib Mineral Petrol, 132: 139–148
Tsay A, Zajacz Z, Sanchez-Valle C. 2014. Efficient mobiliztion and fractionation of rare-earth elements by aqueous fluids upon slab dehydration. Earth Planet Sci Lett, 398: 101–112
Tsujimori T, Ernst W. 2013. Lawsonite blueschists and lawsonite eclogites as proxies for palaeo-subduction zone processes: A review. J Metamorph Geol, 32: 437–454
Tsujimori T, Sisson V B, Liou J G, Harlow G E, Sorensen S S. 2006. Very-low-temperature record of the subduction process: A review of worldwide lawsonite eclogites. Lithos, 92: 609–624
Ulmer P, Trommsdorff V. 1995. Serpentine stability to mantle depths and subduction-related magmatism. Science, 268: 858–861
van Keken P E, Kiefer B, Peacock S M. 2002. High-resolution models of subduction zones: Implications for mineral dehydration reactions and the transport of water into the deep mantle. Geochem Geophy Geosy, 3, doi: 10.1029/2001GC000256
Vlastélic I, Koga K, Chauvel C, Jacques G, Télouk P. 2009. Survival of lithium isotopic heterogeneities in the mantle supported by HIMU-lavas from Rurutu Island, Austral Chain. Earth Planet Sci Lett, 286: 456–466
Vigouroux N, Wallace P J, Williams-Jones G, Kelley K, Kent A J, Williams-Jones A E. 2012. The sources of volatile and fluid-mobile elements in the Sunda arc: A melt inclusion study from Kawah Ijen and Tambora volcanoes, Indonesia. Geochem Geophys Geosyst, doi: 10.1029/2012GC004192
Wallace P J. 2005. Volatiles in subduction zone magmas: Concentrations and fluxes based on melt inclusion and volcanic gas data. J Volcanol Geotherm Res, 140: 217–240
Wallace P J, Edmonds M. 2011. The sulfur budget in magmas: Evidence from melt inclusions, submarine glasses, and volcanic gas emissions. Rev Mineral Geochem, 73: 215–246
Wallis S, Tsuboi M, Suzuki K, Fanning M, Jiang L, Tanaka T. 2005. Role of partial melting in the evolution of the Sulu (eastern China) ultra high-pressure terrane. Geology, 33: 129–132
Wang S J, Teng F Z, Li S G, Hong J A. 2014. Magnesium isotopic systematic of mafic rocks during continental subduction. Geochim Cosmochim Acta, 143: 34–48
Wang S J, Teng F Z, Williams H M, Li S G. 2012. Magnesium isotopic variations in cratonic eclogites: Origins and implications. Earth Planet Sci Lett, 359: 219–226
Webster J D, Botcharnikov R E. 2011. Distribution of sulfur between melt and fluid in SOHC-Cl-bearing magmatic systems at shallow crustal pressures and temperatures. Rev Mineral Geochem, 73: 247–283
Wei C, Clarke G. 2011. Calculated phase equilibria for MORB compositions: A reappraisal of the metamorphic evolution of lawsonite eclogite. J Metamorph Geol, 29: 939–952
Whitney D L, Davis, P B. 2006. Why is lawsonite eclogite so rare? Metamorphism and preservation of lawsonite eclogite, Sivrihisar, Turkey. Geology, 34: 473–476
Wunder B, Meixner A, Romer R L, Heinrich W. 2006. Temperature-dependent isotopic fractionation of lithium between clinopyroxene and high-pressure hydrous fluids. Contrib Mineral Petrol, 151: 112–120
Wunder B, Melzer S. 2003. Experimental evidence on phlogopitic mantle metasomatism induced by phengite dehydration. Eur J Mineral, 15: 641–647
Wunder B, Meixner A, Romer R L, Feenstra A, Schettler G, Heinrich W. 2007. Lithium isotope fractionation between Li-bearing staurolite, Li-mica and aqueous fluids: An experimental study. Chem Geol, 238: 277–290
Wunder B, Schreyer W. 1997. Antigorite: High-pressure stability in the system MgO-SiO2-H2O (MSH). Lithos, 41: 213–227
Wykes J L, Mavrogenes J A. 2005. Hydrous sulfide melting: Experimental evidence for the solubility of H2O in sulfide melts. Econ Geol, 100: 157–164
Wyllie P J, Sekine T. 1982. The formation of mantle phlogopite in subduction zone hybridization. Contrib Mineral Petrol, 79: 375–380
Xia Q X, Zheng Y F, Hu Z C. 2010. Trace elements in zircon and coexisting minerals from low-T/UHP metagranite in the Dabie orogen: Implications for action of supercritical fluid during continental subduction-zone metamorphism. Lithos 114, 385–412
Xia Q X, Zheng Y F, Zhou L G. 2008. Dehydration and melting during continental collision: Constraints from element and isotope geochemistry of low-T/UHP granitic gneiss in the Dabie orogen. Chem Geol, 247, 36–65
Xiao Y, Teng F Z, Zhang H F, Yang W. 2013. Large magnesium isotope fractionation in peridotite xenoliths from eastern North China craton: Product of melt-rock interaction. Geochim Cosmochim Acta, 115: 241–261
Xiao Y L, Hoefs J, Hou Z H, Simon K, Zhang Z M. 2001. Geochemical constraints of the eclogite and granulite facies metamorphism as recognized in the Raobazhai complex from North Dabie Shan, China. J Metamorph Geol, 19: 3–19
Xiao Y L, Romer R L, Hoefs J, Meixner A. 2007. Li and B isotope characteristics of ultrahigh-pressure metamorphic rocks from Sulu, China. Geochim Cosmochim Acta, 71: A1132
Xiao Y L, Hoefs J, Hou Z H, Simon K, Zhang Z M. 2011b. Fluid/rock interaction and mass transfer in continental subduction zones: Constraints from trace elements and isotopes (Li, B, O, Sr, Nd, Pb) in UHP rocks from the Chinese Continental Scientific Drilling Program, Sulu, East China. Contrib Mineral Petrol, 162: 797–819
Xiao Y L, Hoefs J, van den Kerkhof A M, Fiebig J, Zheng Y F. 2000. Fluid history of UHP metamorphism in Dabie Shan, China: A fluid inclusion and oxygen isotope study on the coesite-bearing eclogite from Bixiling. Contrib Mineral Petrol, 139: 1–16
Xiao Y L, Hoefs J, van den Kerkhof A M, Simon K, Fiebig J, Zheng Y F. 2002. Fluid evolution during HP and UHP metamorphism in Dabie Shan, China: Constraints from mineral chemistry, fluid inclusions and stable isotopes. J Petrol, 43: 1505–1527.
Xiao Y L, Hoefs J, Kronz A. 2005. Compositionally zoned Cl-rich amphiboles from North Dabie Shan, China: Monitor of high-pressure metamorphic fluid/rock interaction processes. Lithos, 81: 279–295
Xiao Y L, Huang J, Liu L, Li D Y. 2011a. Rutile: An important" reservoir" for geochemical information. Acta Petrol Sin 27, 398–416.
Xiao Y L, Zhang Z M, Hoefs J, van den Kerkhof A. 2006a. Ultrahigh-pressure metamorphic rocks from the Chinese Continental Scientific Drilling Project: II Oxygen isotope and fluid inclusion distributions through vertical sections. Contrib Mineral Petrol, 152: 443–458
Xiao Y L, Sun W D, Hoefs J, Simon K, Zhang Z M, Li S G, Hofmann A W. 2006b. Making continental crust through slab melting: Constraints from niobium-tantalum fractionation in UHP metamorphic rutile. Geochim Cosmochim Acta, 70: 4770–4782
Xiong X L, Adam J, Green T H. 2005. Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: Implications for TTG genesis. Chem Geol, 218: 339–359
Xiong X L, Keppler H, Audétat A, Ni H W, Sun W D, Li Y. 2011. Partitioning of Nb and Ta between rutile and felsic melt and the fractionation of Nb/Ta during partial melting of hydrous metabasalt. Geochim Cosmochim Acta, 75, 1673–1692
Xu S T, Okay A I, Ji S Y, Sengor A M C, Su W, Liu Y C, Jiang L L. 1992. Diamond from the Dabieshan metamorphic rocks and its implication for tectonic setting. Science, 256: 80–82
Yang W, Teng F Z, Zhang H F. 2009. Chondritic magnesium isotopic composition of the terrestrial mantle: A case study of peridotite xenoliths from the North China craton. Earth Planet Sci Lett, 288: 475–482
Yang W, Teng F Z, Zhang H F, Li S G. 2012b. Magnesium isotopic systematic of continental basalts from the North China craton: Implications for tracing subducted carbonate in the mantle. Chem Geol, 328: 185–194
Yang J J, Powell R. 2008. Ultrahigh-pressure garnet peridotites from the devolatilization of sea-floor hydrated ultramafic rocks. J Metamorph Geol, 26:695–716
Yang Q L, Zhao Z F, Zheng Y F. 2012. Slab-mantle interaction in continental subduction channel: Geochemical evidence from Mesozoic gabbroic intrusives in southeastern North China. Lithos, 155: 442–460
Yaxley G M, Green D H. 1998. Reactions between eclogite and peridotite: Mantle refertilisation by subduction of oceanic crust. Schweizerische Mineralogische Und Petrographische Mitteilungen, 78: 243–255
Ye K, Cong B, Ye D. 2000. The possible subduction of continental material to depths greater than 200 km. Nature, 407: 734–736
Yogodzinski G, Lees J, Churikova T, Dorendorf F, Wöerner G, Volynets O. 2001. Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges. Nature, 409: 500–504
Zack T, Kronz A, Foley S F, et al. 2002. Trace element abundances in rutiles from eclogites and associated garnet mica schists. Chem Geol, 184, 97–122
Zack T, Tomascak P B, Rudnick R L, Dalpé C, McDonough W F. 2003. Extremely light Li in orogenic eclogites: The role of isotope fractionation during dehydration in subducted oceanic crust. Earth Planet Sci Lett, 208: 279–290
Zack T, Moraes R, Kronz A, 2004. Temperature dependence of Zr in rutile: Empirical calibration of a rutile thermometer. Contrib Mineral Petrol, 148: 471–488
Zanetti A, Mazzucchelli M, Rivalenti G, Vannucci R. 1999. The Finero phlogopite-peridotite massif: An example of subduction-related metasomatism. Contrib Mineral Petrol, 134: 107–122
Zhang H F, Sun M, Zhou X H, Fan W M, Zhai M G, Yin J F. 2002. Mesozoic lithosphere destruction beneath the North China Craton: Evidence from major-, trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contrib Mineral Petrol 144: 241–254
Zhang H F, Sun M, Zhou X H, Zhou M F, Fan W M, Zheng J P. 2003. Secular evolution of the lithosphere beneath the eastern North China Craton: Evidence from Mesozoic basalts and high-Mg andesites. Geochim Cosmochim Acta, 67: 4373–4387
Zhang H F, Sun Y L, Tang Y J, Xiao Y, Zhang W H, Zhao X M, Santosh M, Menzies M A. 2012. Melt-peridotite interaction in the Pre-Cambrian mantle beneath the western North China Craton: Petrology, geochemistry and Sr, Nd and Re isotopes. Lithos, 149: 100–114
Zhang R Y, Liou J G, Yang J S, Yui T F. 2000. Petrochemical constraints for dual origin of garnet peridotites from the Dabie-Sulu UHP terrane, eastern-central China. J Metamorph Geol, 18: 149–166
Zhang R Y, Li T, Rumble D, Yui T F, Li L, Yang J S, Pan Y, Liou J G. 2007. Multiple metasomatism in Sulu ultrahigh-P garnet peridotite constrained by petrological and geochemical investigations. J Metamorph Geol, 25: 149–164
Zhang Z M, Shen K, Sun W D, Liu Y S, Liou J, Shi C, Wang J L. 2008. Fluids in deeply subducted continental crust: Petrology, mineral chemistry and fluid inclusion of UHP metamorphic veins from the Sulu orogen, eastern China. Geochim Cosmochim Acta, 72: 3200–3228
Zhang Z M, Dong X, Liou J Q, Liu F, Wang W, Yui F. 2011. Metasomatism of garnet peridotite from Jiangzhuang, southern Sulu UHP belt: Constraints on the interactions between crust and mantle rocks during subduction of continental lithosphere. J Metamorph Geol, 29: 917–937
Zhao Z F, Zheng Y F, Chen R X, Xia Q X, Wu Y B. 2007. Element mobility in mafic and felsic ultrahigh-pressure metamorphic rocks during continental collision. Geochim Cosmochim Acta, 71, 5244–5266
Zhao Z F, Dai L Q, Zheng Y F. 2013. Postcollisional mafic igneous rocks record crust-mantle interaction during continental deep subduction. Sci Rep, 3, doi: 10.1038/srep03413
Zheng J P, Zhang R Y, Griffin W L, Liou J Q, O’Reilly S Y. 2005. Heterogeneous and metasomatized mantle recorded by trace elements in minerals of the Donghai garnet peridotites, Sulu UHP terrane, China. Chem Geol, 221: 243–259
Zheng J P, Griffin W L, O'Reilly S Y, Zhang M, Pearson N. 2006a. Zircons in mantle xenoliths record the Triassic Yangtze-North China continental collision. Earth Planet Sci Lett, 247: 130–142
Zheng J P, Griffin W L, O’Reilly S Y, Yang J, Zhang R Y. 2006b. A refractory mantle protolith in younger continental crust, east-central China: Age and composition of zircon in the Sulu ultrahigh-pressure peridotite. Geology, 34: 705–708
Zheng J P, Sun M, Griffin W L, Zhou M F, Zhao G C, Robinson P, Tang H Y, Zhang Z H. 2008. Age and geochemistry of contrasting peridotite types in the Dabie UHP belt, eastern China: Petrogenetic and geodynamic implications. Chem Geol, 247: 282–304
Zheng Y F. 2009. Fluid regime in continental subduction zones: Petrological insights from ultrahigh-pressure metamorphic rocks. J Geol Soc, 166: 763–782
Zheng Y F, Fu B, Gong B, Li L. 2003. Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China: Implications for geodynamics and fluid regime. Earth-Sci Rev, 62: 105–161
Zheng Y F, Chen R X., Zhao Z F., 2009. Chemical geodynamics of continental subduction-zone metamorphism: Insights from studies of the Chinese Continental Scientific Drilling (CCSD) core samples. Tectonophysics, 475: 327–358
Zheng Y F, Xia Q X, Chen R X, Gao X Y. 2011. Partial melting, fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision. Earth-Sci Rev, 107: 342–374
Zheng Y F. 2012. Metamorphic chemical geodynamics in continental subduction zones. Chem Geol, 328: 5–48
Zheng Y F, Hermann J. 2014. Geochemistry of continental subductionzone fluids. Earth Planets Space, 66: 93, doi: 10.1186/1880-5981-66-93
Zheng Y F, Zhao Z F, Chen Y X. 2013. Continental subduction channel processes: Plate interface interaction during continental collision. Chin Sci Bull, 58: 2233–2239
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Xiao, Y., Sun, H., Gu, H. et al. Fluid/melt in continental deep subduction zones: Compositions and related geochemical fractionations. Sci. China Earth Sci. 58, 1457–1476 (2015). https://doi.org/10.1007/s11430-015-5149-8
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11430-015-5149-8