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
[2]
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
[3]
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
[4]
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
[5]
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
[6]
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
[7]
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
[8]
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
[9]
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
[10]
Davies J H, Stevenson D J. 1992. Physical model of source region of subduction zone volcanics. J Geophys Res, 97: 2037-2070
[11]
Defant M J, Drummond M S. 1990. Derivation of some modern arc magmas by melting of young subducted lithosphere. Nature, 347: 662-665
[12]
Deschamps F, Godard M, Guillot S, Hattori K. 2013. Geochemistry of subduction zone serpentinites: A review. Lithos, 178: 96-127
[13]
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
[14]
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
[15]
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
[16]
Eggler D H, Burnham C W. 1984. Solution of H2O in diopside melts—A thermodynamic model. Contrib Mineral Petrol, 85: 58-66
[17]
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
[18]
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
[19]
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
[20]
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
[21]
Foley S, Tiepolo M, Vannucci R. 2002. Growth of early continental crust controlled by melting of amphibolite in subduction zones. Nature, 417: 837-840
[22]
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
[23]
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
[24]
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
[25]
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
[26]
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
[27]
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
[28]
Gaetani G A, Grove T L. 1998. The influence of water on melting of mantle peridotite. Contrib Mineral Petrol, 131: 323-346
[29]
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
[30]
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
[31]
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
[32]
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
[33]
Gill J B. 1981. Geophysical Setting of Volcanism at Convergent Plate Boundaries, Orogenic Andesites and Plate Tectonics. Berlin: Springer. 44-63
[34]
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
[35]
Green D H, Hibberson W O, Kovács I, Rosenthal A. 2010. Water and its influence on the lithosphere-asthenosphere boundary. Nature, 467: 448-451
[36]
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
[37]
Grove T L, Elkins-Tanton LT, 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
[38]
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
[39]
Gorman P J, Kerrick D, Connolly J. 2006. Modeling open system metamorphic decarbonation of subducting slabs. Geochem Geophys Geosyst, 7, doi: 10.1029/2005GC001125
[40]
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
[41]
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
[42]
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
[43]
Hacker B R. 2008. H2O subduction beyond arcs. Geochem Geophs Geosyst, 9, doi: 10.1029/2007GC001707
[44]
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
[45]
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
[46]
Hermann J, Rubatto D. 2009. Accessory phase control on the trace element signature of sediment melts in subduction zones. Chem Geol, 265: 512-526
[47]
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
[48]
Hermann J, Spandler C J. 2008. Sediment melts at sub-arc depths: An experimental study. J Petrol, 49: 717-740
[49]
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
[50]
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
[51]
Hermann J, Zheng Y F, Rubatto D. 2013. Deep fluids in subducted continental crust. Elements, 9: 281-287
[52]
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
[53]
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
[54]
Honma H, Itihara Y. 1981. Distribution of ammonium in minerals of metamorphic and granitic rocks. Geochim Cosmochim Acta, 45: 983-988
[55]
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
[56]
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
[57]
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
[58]
Jarrard R D. 2003. Subduction fluxes of water, carbon dioxide, chlorine, and potassium. Geochem Geophs Geosyst, 4, doi: 10.1029/ 2002GC000392
[59]
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
[60]
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
[61]
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
[62]
John T, Klemd R, Gao J, Garbe-Sch?nberg 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
[63]
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
[64]
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
[65]
Kawamoto T, Yoshikawa M, Kumagai Y, Mirabueno M H T, 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
[66]
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. Geophys Monograph, 138: 293-311
[67]
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
[68]
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
[69]
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
[70]
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
[71]
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
[72]
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
[73]
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
[74]
Krawczynski. 2011. Experimental studies of melting and crystallization processes in planetary interiors. Doctoral Dissertation. Massachusetts Institute of Technology. 202
[75]
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
[76]
Kushiro K. 1990. Partial melting of mantle wedge and evolution of island arc crust. J Geophys Res, 95: 15929-15939
[77]
Labrousse L, Prouteau G, Ganzhorn A C. 2011. Continental exhumation triggered by partial melting at ultrahigh pressure. Geology, 39: 1171-1174
[78]
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
[79]
Li W Y, Teng F Z, Wing B A, Xiao Y L. 2014. Limited magnesium isotope fractionation during metamorphic dehydration in metapelites from the Onawa contact aureole, Maine. Geochem Geophys Geosyst, 15: 408-415
[80]
Li W Y, Teng F Z, Xiao Y L, Huang J. 2011. High-temperature inter-mineral magnesium isotope fractionation in eclogite from the Dabie orogen, China. Earth Planet Sci Lett, 304: 224-230
[81]
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
[82]
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
[83]
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
[84]
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
[85]
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
[86]
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
[87]
Malaspina N, Hermann J, Scambelluri M. 2009. Fluid/mineral interaction in UHP garnet peridotite. Lithos, 107: 38-52
[88]
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
[89]
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
[90]
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
[91]
Manning C E. 1994. The solubility of quartz in H2O in the lower crust and upper-mantle. Geochim Cosmochim Acta, 58: 4831-4839
[92]
Manning C E. 2004. The chemistry of subduction-zone fluids. Earth Planet Sci Lett, 223: 1-16
[93]
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
[94]
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
[95]
Marschall H R, Schumacher J. 2012. Arc magmas sourced from melange diapirs in subduction zones. Nat Geosci, 5: 862-867
[96]
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
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
[101]
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
[102]
Ague J J, Nicolescu S. 2014. Carbon dioxide released from subduction zones by fluid-mediated reactions. Nat Geosci, 7: 355-360
[103]
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
[104]
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
[105]
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
[106]
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
[107]
Alt J C, Shanks W C. 2011. Microbial sulfate reduction and the sulfur budget for a complete section of altered oceanic basalts, IODP Hole 1256D (eastern Pacific). Earth Planet Sci Lett, 310: 73-83
[108]
Aulbach S, O’Reilly S Y, Pearson N J. 2011. Constraints from eclogite and MARID xenoliths on origins of mantle Zr/Hf-Nb/Ta variability. Contrib Mineral Petrol, 162: 1047-1062
[109]
Auzanneau E, Vielzeuf D, Schmidt M. 2006. Experimental evidence of decompression melting during exhumation of subducted continental crust. Contrib Mineral Petrol, 152: 125-148
[110]
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
[111]
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
[112]
Bebout G E. 2007. Metamorphic chemical geodynamics of subduction zones. Earth Planet Sci Lett, 260: 373-393
[113]
Bebout G E, Marilyn L F, Cartigny P. 2013a. Nitrogen: Highly volatile yet surprisingly compatible. Elements, 9: 333-338
[114]
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
[115]
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
[116]
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
[117]
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
[118]
Blundy J, Cashman K, Humphreys M. 2006. Magma heating by decompression-driven crystallization beneath and esite volcanoes. Nature, 443: 76-80
[119]
Blundy J, Wood B. 2003. Partitioning of trace elements between crystals and melts. Earth Planet Sci Lett, 210: 383-397
[120]
Bourdon B, Tipper E T, Fitoussi C, Stracke A. 2010. Chondritic Mg isotope composition of the Earth. Geochim Cosmochim Acta, 74: 5069-5083
[121]
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
[122]
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
[123]
Burton M R, Sawyer G M, Granieri D. 2013. Deep carbon emissions from volcanoes. Rev Mineral Geochem, 75: 323-354
[124]
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
[125]
Canfield D E. 2004. The evolution of the Earth surface sulfur reservoir. Am J Sci, 304: 839-861
[126]
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
[127]
Cartigny P, Marty B. 2013. Nitrogen Isotopes and Mantle Geodynamics: The Emergence of Life and the Atmosphere-Crust-Mantle Connection. Elements, 9: 359-364
[128]
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
[129]
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
[130]
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
[131]
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
[132]
McCammon C. 2005. The paradox of mantle redox. Science, 308: 807-808
[133]
Médard E, Grove T L. 2006. Early hydrous melting and degassing of the Martian interior. J Geophys Res, 111, doi: 10.1029/2006JE002742
[134]
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
[135]
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
[136]
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
[137]
Münker C, Pf?nder 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
[138]
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
[139]
Pf?nder 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
[140]
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
[141]
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
[142]
Parkinson I J, Arculus R J. 1999. The redox state of subduction zones: Insights from arc-peridotites. Chem Geol, 160: 409-423
[143]
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
[144]
Pawley A. 2003. Chlorite stability in mantle peridotite: The reaction clinochlore+enstatite=forsterite+pyrope+H2O. Contrib Mineral Petrol, 144: 449-456
[145]
Peacock S M. 1990. Fluid processes in subduction zones. Science, 248: 329-337
[146]
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
[147]
Plank T, Cooper L B, Manning C E. 2009. Emerging geothermometers for estimating slab surface temperatures. Nat Geosci, 2: 611-615
[148]
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
[149]
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
[150]
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
[151]
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
[152]
Rapp R P, Shimizu N, Norman M D. 2003. Growth of early continental crust by partial melting of eclogite. Nature, 425: 605-609
[153]
Richter F. 2003. Isotope fractionation by chemical diffusion between molten basalt and rhyolite. Geochim Cosmochim Acta, 67: 3905-3923
[154]
Richter F M, McKenzie D P. 1978. Simple plate models of mantle convection. J Geophys, 44: 441-471
[155]
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
[156]
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
[157]
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
[158]
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
[159]
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
[160]
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
[161]
Shreve R L, Cloos M. 1986. Dynamics of sediment subduction, mélange formation, and prism accretion. J Geophys Res, 91: 10229-10245
[162]
Simon A C, Ripley E M. 2011. The role of magmatic sulfur in the formation of ore deposits. Rev Mineral Geochem, 73: 513-578
[163]
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
[164]
Sinogeikin S V, Schilling F R, Bass J D. 2000. Single crystal elasticity of lawsonite. Am Mineral, 85: 1834-1837
[165]
Sisson T W, Grove T L. 1993. Temperatures and H2O contents of low-MgO high-alumina basalts. Contrib Mineral Petrol, 113: 167-184
[166]
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
[167]
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
[168]
Smith D C. 1984. Coesite in clinopyroxene in the Caledonides and its implications for geodynamics. Nature, 310: 641-644
[169]
Sobolev N V, Shatsky V S. 1990. Diamond inclusions in garnets from metamorphic rocks: A new environment for diamond formation. Nature, 343: 742-746
[170]
Spandler C, Pirard C. 2013. Element recycling from subducting slabs to arc crust: A review. Lithos, 170: 208-223
[171]
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
[172]
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
[173]
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
[174]
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
[175]
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
[176]
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
[177]
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
[178]
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
[179]
Tatsumi Y, Eggins S. 1995. Subduction Zone Magmatism, 1. Cambridge: Blackwell Science
[180]
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
[181]
Teng F Z, Li W Y, Ke S, Marty B, Dauphas N, Huang S, Wu F Y, Pourmand A. 2010a. Magnesium isotopic composition of the Earth and chondrites. Geochim Cosmochim Acta, 74: 4150-4166
[182]
Thorkelson D J, Breitsprecher K. 2005. Partial melting of slab window margins: Genesis of adakitic and non-adakitic magmas. Lithos, 79: 25-41
[183]
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
[184]
Till C B, Grove T L, Withers A C. 2012. The beginnings of hydrous mantle wedge melting. Contrib Mineral Petrol, 163: 669-688
[185]
Tomlinson E L, Mueller W, Eimf. 2009. A snapshot of mantle metasomatism: Trace element analysis of coexisting fluid (LA-ICP-MS) and silicate (SIMS) inclusions in fibrous diamonds. Earth Planet Sci Lett, 279: 362-372
[186]
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
[187]
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
[188]
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
[189]
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
[190]
Ulmer P, Trommsdorff V. 1995. Serpentine stability to mantle depths and subduction-related magmatism. Science, 268: 858-861
[191]
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
[192]
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
[193]
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
[194]
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
[195]
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
[196]
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
[197]
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
[198]
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
[199]
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
[200]
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
[201]
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
[202]
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
[203]
Wunder B, Melzer S. 2003. Experimental evidence on phlogopitic mantle metasomatism induced by phengite dehydration. Eur J Mineral, 15: 641-647
[204]
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
[205]
Wunder B, Schreyer W. 1997. Antigorite: High-pressure stability in the system MgO-SiO2-H2O (MSH). Lithos, 41: 213-227
[206]
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
[207]
Wyllie P J, Sekine T. 1982. The formation of mantle phlogopite in subduction zone hybridization. Contrib Mineral Petrol, 79: 375-380
[208]
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
[209]
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
[210]
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
[211]
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
[212]
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
[213]
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
[214]
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
[215]
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.
[216]
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
[217]
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
[218]
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
[219]
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
[220]
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
[221]
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 Dabie-Shan metamorphic rocks and its implication for tectonic setting. Science, 256: 80-82
[222]
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
[223]
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
[224]
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
[225]
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
[226]
Yaxley G M, Green D H. 1998. Reactions between eclogite and peridotite: Mantle refertilisation by subduction of oceanic crust. Schweiz Miner Petrog, 78: 243-255
[227]
Ye K, Cong B, Ye D. 2000. The possible subduction of continental material to depths greater than 200 km. Nature, 407: 734-736
[228]
Yogodzinski G, Lees J, Churikova T, Dorendorf F, W?erner G, Volynets O. 2001. Geochemical evidence for the melting of subducting oceanic lithosphere at plate edges. Nature, 409: 500-504
[229]
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
[230]
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
[231]
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
[232]
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
[233]
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
[234]
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
[235]
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
[236]
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
[237]
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
[238]
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
[239]
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
[240]
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
[241]
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
[242]
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
[243]
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
[244]
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
[245]
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
[246]
Zheng Y F. 2009. Fluid regime in continental subduction zones: Petrological insights from ultrahigh-pressure metamorphic rocks. J Geol Soc, 166: 763-782
[247]
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
[248]
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
[249]
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
[250]
Zheng Y F. 2012. Metamorphic chemical geodynamics in continental subduction zones. Chem Geol, 328: 5-48
[251]
Zheng Y F, Hermann J. 2014. Geochemistry of continental subduction-zone fluids. Earth Planets Space, 66: 93, doi: 10.1186/1880-5981-66-93