Agranier A, Lee C T A, Li Z X A, Leeman W P. 2007. Fluid-mobile element budgets in serpentinized oceanic lithospheric mantle: insights from B, As, Li, Pb, PGEs and Os isotopes in the Feather River Ophiolite, California. Chemical Geology, 245(3-4): 230~241.
Agrinier P, Cannat M. 1997. Oxygen-isotope constraints on serpentinization processes in ultramafic rocks from the Mid-Atlantic Ridge(23°N). In: Karson J A, Cannat M, Miller D J, Elthon D, eds. Proceedings of the Ocean Drilling Program, Scientific Results, 153: 381~388.
Ali S, Ntaflos T, Sami M. 2021. Geochemistry of Khor Um-Safi ophiolitic serpentinites, central eastern desert, Egypt: implications for neoproterozoic arc-basin system in the Arabian-Nubian shield. Geochemistry, 81(1): 125690.
Alt J C, Shanksiii W. 2006. Stable isotope compositions of serpentinite seamounts in the Mariana forearc: serpentinization processes, fluid sources and sulfur metasomatism. Earth and Planetary Science Letters, 242(3-4): 272~285.
Alt J C, Schwarzenbach E M, Früh-Green G L, Shanks W C, Bernasconi S M, Garrido C J, Crispini L, Gaggero L, Padrón-Navarta J A, Marchesi C. 2013. The role of serpentinites in cycling of carbon and sulfur: seafloor serpentinization and subduction metamorphism. Lithos, 178: 40~54.
Andreani M, Escartin J, Delacour A, Ildefonse B, Godard M, Dyment J, Fallick A E, Fouquet Y. 2014. Tectonic structure, lithology, and hydrothermal signature of the rainbow massif (mid-Atlantic ridge 36° 14′ N). Geochemistry, Geophysics, Geosystems, 15(9): 3543~3571.
Angiboust S, Wolf S, Burov E, Agard P, Yamato P. 2012. Effect of fluid circulation on subduction interface tectonic processes: insights from thermo-mechanical numerical modelling. Earth and Planetary Science Letters, 357: 238~248.
Anselmi B, Mellini M, Viti C. 2000. Chlorine in the Elba, Monti Livornesi and Murlo serpentines: evidence for sea-water interaction. European Journal of Mineralogy, 12(1): 137~146.
Augustin N, Lackschewitz K S, Kuhn T, Devey C W. 2008. Mineralogical and chemical mass changes in mafic and ultramafic rocks from the Logatchev hydrothermal field (MAR 15°N). Marine Geology, 256(1-4): 18~29.
Augustin N, Paulick H, Lackschewitz K S, Eisenhauer A, Garbe-Schönberg D, Kuhn T, Botz R, Schmidt M. 2012. Alteration at the ultramafic-hosted Logatchev hydrothermal field: constraints from trace element and Sr-O isotope data. Geochemistry, Geophysics, Geosystems, 13(3), doi: 10. 1029/2011GC003903.
Audétat A, Günther D, Heinrich C A. 2000. Magmatic-hydrothermal evolution in a fractionating granite: a microchemical study of the Sn-WF-mineralized mole granite (Australia). Geochimica et Cosmochimica Acta, 64(19): 3373~3393.
Aziz N R H, Aswad K J A, Koyi H A. 2011. Contrasting settings of serpentinite bodies in the northwestern Zagros Suture Zone, Kurdistan region, Iraq. Geological Magazine, 148(5-6): 819~837.
Babechuk M G, Kamber B S, Greig A, Canil D, Kodolányi J. 2010. The behaviour of tungsten during mantle melting revisited with implications for planetary differentiation time scales. Geochimica et Cosmochimica Acta, 74(4): 1448~1470.
Bali E, Keppler H, Audetat A. 2012. The mobility of W and Mo in subduction zone fluids and the Mo-W-Th-U systematics of island arc magmas. Earth and Planetary Science Letters, 351: 195~207.
Barnes J D, Beltrando M, Lee C T A, Cisneros M, Loewy S, Chin E. 2014. Geochemistry of Alpine serpentinites from rifting to subduction: a view across paleogeographic domains and metamorphic grade. Chemical Geology, 389: 29~47.
Barnes J D, Manning C, Scambelluri M, Selverstone J. 2018. The behavior of halogens during subduction zone processes. The Role of Halogens in Terrestrial and Extraterrestrial Geochemical Processes. Berlin: Springer, 545~590.
Bebout G E. 2007. Metamorphic chemical geodynamics of subduction zones. Earth and Planetary Science Letters, 260(3-4): 373~393.
Black J R, Kavner A, Schauble E A. 2011. Calculation of equilibrium stable isotope partition function ratios for aqueous zinc complexes and metallic zinc. Geochimica et Cosmochimica Acta, 75(3): 769~783.
Blanco-Quintero I, Proenza J A, Garcia-Casco A, Tauler E, Gali S. 2011. Serpentinites and serpentinites within a fossil subduction channel: La Corea mélange, Eastern Cuba. Geologica Acta, 9: 389~405.
Bonatti E. 1976. Serpentinite protrusions in the oceanic crust. Earth and Planetary Science Letters, 32(2): 107~113.
Boschi C, Bonatti E, Ligi M, Brunelli D, Cipriani A, Dallai L, D'Orazio M, FrühGreen G L, Tonarini S, Barnes J D, Bedini R M. 2013. Serpentinization of mantle peridotites along an uplifted lithospheric section, mid Atlantic ridge at 11° N. Lithos, 178: 3~23.
Bostock M G, Hyndman R D, Rondenay S, Peacock S M. 2002. An inverted continental Moho and serpentinization of the forearc mantle. Nature, 417(6888): 536~538.
Bouilhol P, Magni V, van Hunen J, Kaislaniemi L. 2015. A numerical approach to melting in warm subduction zones. Earth and Planetary Science Letters, 411: 37~44.
Bouilhol P, Debret B, Inglis E C, Warembourg M, Grocolas T, Rigaudier T, Villeneuve J, Burton K W. 2022. Decoupling of inorganic and organic carbon during slab mantle devolatilisation. Nature Communications, 13(1): 1~10.
Bowen N L, Tuttle O F. 1949. The system MgO-SiO2-H2O. Geological Society of America Bulletin, 60(3): 439~460.
Brzozowski M J, Good D J, Wu Changzhi, Li Weiqiang. 2021. Cu isotope systematics of conduit-type Cu-PGE mineralization in the Eastern Gabbro, Coldwell Complex, Canada. Mineralium Deposita, 56(4): 707~724.
Cannaò E, Scambelluri M, Agostini S, Tonarini S, Godard M. 2016. Linking serpentinite geochemistry with tectonic evolution at the subduction plate-interface: the Voltri Massif case study(Ligurian Western Alps, Italy). Geochimica et Cosmochimica Acta, 190: 115~133.
Cannat M, Mevel C, Maia M, Deplus C, Durand C, Gente P, Agrinier P, Belarouchi A, Dubuisson G, Humler E, Reynolds J. 1995. Thin crust, ultramafic exposures, and rugged faulting patterns at the Mid-Atlantic Ridge(22°-24°N). Geology, 23(1): 49~52.
Chalot-Prat F, Ganne J, Lombard A. 2003. No significant element transfer from the oceanic plate to the mantle wedge during subduction and exhumation of the Tethys lithosphere (Western Alps). Lithos, 69(3-4): 69~103.
Chen Yixiang. 2021. The fractionation behavior of Mg and Fe isotopes during serpentinite dehydration in subduction zones: progress and prospect. Bulletin of Mineralogy, Petrology and Geochemistry, 40(5): 1034~1048 (in Chinese with English abstract).
Chen Yixiang, Lu Wenning, He Yongsheng, Schertl H P, Zheng Yongfei, Xiong Jiawei, Zhou Kun. 2019. Tracking Fe mobility and Fe speciation in subduction zone fluids at the slab-mantle interface in a subduction channel: a tale of whiteschist from the Western Alps. Geochimica et Cosmochimica Acta, 267: 1~16.
Chen Yixiang, Demény A, Schertl H P, Zheng Yongfei, Huang Fang, Zhou Kun, Jin Qizhen, Xia Xiaoping. 2020. Tracing subduction zone fluids with distinct Mg isotope compositions: insights from high-pressure metasomatic rocks(leucophyllites)from the Eastern Alps. Geochimica et Cosmochimica Acta, 271: 154~178.
Chen Zuxing, Chen Jiubin, Zeng Zhigang, Soh Tamehe L, Zhang Ting, Zhang Yuxiang, Yin Xuebo, Wang Xiaoyuan, Chen Shuai, Shuai Wangcai. 2021. Zinc isotopes of the mariana and ryukyu arc-related lavas reveal recycling of forearc serpentinites into the subarc mantle. Journal of Geophysical Research: Solid Earth, 126(11): e2021JB022261.
Coleman R G, Keith T E. 1971. A chemical study of serpentinization—Burro Mountain, California. Journal of Petrology, 12(2): 311~328.
Cooper G F, Macpherson C G, Blundy J D, Maunder B, Allen R W, Goes S, Collier J S, Bie L, Harmon N, Hicks S P, Iveson A A, Prytulak J, Rietbrock A, Rychert C A, Davidson J P. 2020. Variable water input controls evolution of the Lesser Antilles volcanic arc. Nature, 582(7813): 525~529.
Craddock P R, Warren J M, Dauphas N. 2013. Abyssal peridotites reveal the near-chondritic Fe isotopic composition of the Earth. Earth and Planetary Science Letters, 365: 63~76.
Crossley R J, Evans K A, Jeon H, Kilburn M R. 2018. Insights into sulfur cycling at subduction zones from in-situ isotopic analysis of sulfides in high-pressure serpentinites and ‘hybrid’ samples from Alpine Corsica. Chemical Geology, 493: 359~378.
Debret B, Koga K T, Nicollet C, Andreani M. 2013. F, Cl and S input via serpentinite in subduction zones: implications for the nature of the fluid released at depth. Terra Nova, 26(2): 96~101.
Debret B, Millet M A, Pons M L, Bouilhol P, Inglis E, Williams H. 2016. Isotopic evidence for iron mobility during subduction. Geology, 44(3): 215~218.
Debret B, Beunon H, Mattielli N, Andreani M, Da Costa I R, Escartin J. 2018. Ore component mobility, transport and mineralization at mid-oceanic ridges: a stable isotopes (Zn, Cu and Fe) study of the rainbow massif (Mid-Atlantic Ridge 36° 14′ N). Earth and Planetary Science Letters, 503: 170~180.
Debret B, Albers E, Walter B, Price R, Barnes J D, Beunon H, Facq S, Gillikin D P, Mattielli N, Williams H. 2019. Shallow forearc mantle dynamics and geochemistry: new insights from IODP Expedition 366. Lithos, 326: 230~245.
Debret B, Reekie C D J, Mattielli N, Beunon H, Ménez B, Savov I, Williams H M. 2020. Redox transfer at subduction zones: insights from Fe isotopes in the Mariana forearc. Geochemical Perspectives Letters, 12: 46~51.
Debret B, Garrido C J, Pons M L, Bouilhol P, Inglis E, López Sánchez-Vizcaíno V, Williams H. 2021. Iron and zinc stable isotope evidence for open-system high-pressure dehydration of antigorite serpentinite in subduction zones. Geochimica et Cosmochimica Acta, 296: 210~225.
Delacour A, Früh-Green G L, Frank M, Gutjahr M, Kelley D S. 2008. Sr- and Nd-isotope geochemistry of the Atlantis Massif (30°N, MAR): implications for fluid fluxes and lithospheric heterogeneity. Chemical Geology, 254(1-2): 19~35.
Deng Jianghong, He Yongsheng, Zartman R E, Yang Xiaoyong, Sun Weidong. 2022. Large iron isotope fractionation during mantle wedge serpentinization: implications for iron isotopes of arc magmas. Earth and Planetary Science Letters, 583: 117423.
Deschamps F, Guillot S, Godard M, Chauvel C, Andreani M, Hattori K. 2010. In situ characterization of serpentinites from forearc mantle wedges: timing of serpentinization and behavior of fluid-mobile elements in subduction zones. Chemical Geology, 269(3-4): 262~277.
Deschamps F, Godard M, Guillot S, Chauvel C, Andreani M, Hattori K, Wunder B, France L. 2012. Behavior of fluid-mobile elements in serpentines from abyssal to subduction environments: examples from Cuba and Dominican Republic. Chemical Geology, 312: 93~117.
Deschamps F, Godard M, Guillot S, Hattori K. 2013. Geochemistry of subduction zone serpentinites: a review. Lithos, 178: 96~127.
Dessimoulie L, Delacour A, Guillaume D, Chevet J, Cottin J-Y. 2020. Major and trace elements exchanges during fluid-rock interaction at ultraslow-spreading oceanic lithosphere: example of the South West Indian Ridge (SWIR). Lithos, 352: 105233.
Dick H J B, Lin J, Schouten H. 2003. An ultraslow-spreading class of ocean ridge. Nature, 426(6965): 405~412.
Evans B W. 2004. The serpentinite multisystem revisited: chrysotile is metastable. International Geology Review, 46(6): 479~506.
Evans B W, Trommsdorff V. 1978. Petrogenesis of garnet lherzolite, Cima di Gagnone, Lepontine Alps. Earth and Planetary Science Letters, 40(3): 333~348.
Evans K A. 2012. The redox budget of subduction zones. Earth-Science Reviews, 113(1-2): 11~32.
Evans K A, Tomkins A G. 2011. The relationship between subduction zone redox budget and arc magma fertility. Earth and Planetary Science Letters, 308(3-4): 401~409.
Evans K A, Frost B R. 2020. Deserpentinization in subduction zones as a source of oxidation in arcs: a reality check. Journal of Petrology, 62(1): 1~32.
Faccenda M, Burlini L, Gerya T V, Mainprice D. 2008. Fault-induced seismic anisotropy by hydration in subducting oceanic plates. Nature, 455(7216): 1097~1100.
Früh-Green G L, Plas A, Lécuyer C. 1996. Petrologic and stable isotope constraints on hydrothermal alteration and serpentinization of the EPR shallow mantle at Hess Deep(site 895). Proceedings of the Ocean Drilling Program, Scientific Results, 147: 255~291.
Fumagalli P, Poli S. 2005. Experimentally determined phase relations in hydrous peridotites to 65 GPa and their consequences on the dynamics of subduction zones. Journal of Petrology, 46(3): 555~578.
Galvez M E, Connolly J A D, Manning C E. 2016. Implications for metal and volatile cycles from the pH of subduction zone fluids. Nature, 539(7629): 420~424.
Garrido C J, López Sánchez-Vizcaíno V, Gómez-Pugnaire M T, Trommsdorff V, Alard O, Bodinier J L, Godard M. 2005. Enrichment of HFSE in chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite: implications for subduction magmatism. Geochemistry, Geophysics, Geosystems, 6(1): https: //doi. org/10. 1029/2004GC000791.
Geldmacher J, Hoernle K, Van Den Bogaard P, Hauff F, Klugel A. 2008. Age and geochemistry of the central American Forearc basement (DSDP leg 67 and 84): insights into Mesozoic arc volcanism and seamount accretion on the fringe of the Caribbean LIP. Journal of Petrology, 49(10): 1781~1815.
Gerya T V, Stöckhert B, Perchuk A L. 2002. Exhumation of high-pressure metamorphic rocks in a subduction channel: a numerical simulation. Tectonics, 21(6): https: //doi. org/10. 1029/2002TC001406.
Gilio M. 2017. Alpine serpentinite geochemistry: a key to unravel subduction accretion at the plate interface. Doctoral thesis of University of Genova, Italy, 308.
Gilio M, Scambelluri M, Agostini S, Godard M, Peters D, Pettke T. 2019. Petrology and geochemistry of serpentinites associated with the ultra-high pressure Lago di Cignana Unit (Italian Western Alps). Journal of Petrology, 60(6): 1229~1262.
González-Jiménez J M, Plissart G, Garrido L N, Padrón-Navarta J A, Aiglsperger T, Romero R, Marchesi C, Moreno-Abril A J, Reich M, Barra F, Morata D. 2017. Titanian clinohumite and chondrodite in antigorite serpentinites from Central Chile: evidence for deep and cold subduction. European Journal of Mineralogy, 29(6): 959~970.
Gorczyk W, Guillot S, Gerya T V, Hattori K. 2007. Asthenospheric upwelling, oceanic slab retreat, and exhumation of UHP mantle rocks: insights from Greater Antilles. Geophysical Research Letters, 34(21): doi: 10. 1029/2007GL031059.
Grove T, Chatterjee N, Parman S, Medard E. 2006. The influence of H2O on mantle wedge melting. Earth and Planetary Science Letters, 249(1-2): 74~89.
Guillot S, Hattori K H, de Sigoyer J. 2000. Mantle wedge serpentinization and exhumation of eclogites: insights from eastern Ladakh, northwest Himalaya. Geology, 28(3): 199~202.
Guillot S, Hattori K H, de Sigoyer J, Nägler T, Auzende A L. 2001. Evidence of hydration of the mantle wedge and its role in the exhumation of eclogites. Earth and Planetary Science Letters, 193(1-2): 115~127.
Guillot S, Hattori K H, Agard P, Schwartz S, Vidal O. 2009. Exhumation processes in oceanic and continental subduction contexts: a review. Subduction Zone Geodynamics, 175~205. Guillot S, Schwartz S, Reynard B, Agard P, Prigent C. 2015. Tectonic significance of serpentinites. Tectonophysics, 646: 1~19.
Hattori K H, Guillot S. 2003. Volcanic fronts form as a consequence of serpentinite dehydration in the forearc mantle wedge. Geology, 31(6): 525~528.
Hattori K H, Guillot S. 2007. Geochemical character of serpentinites associated with high- to ultrahigh-pressure metamorphic rocks in the Alps, Cuba, and the Himalayas: recycling of elements in subduction zones. Geochemistry, Geophysics, Geosystems, 8(9): DOI: 10. 1029/2007GC001594.
Hermann J, Müntener O, Scambelluri M. 2000. The importance of serpentinite mylonites for subduction and exhumation of oceanic crust. Tectonophysics, 327(3-4): 225~238.
Hermann J, Spandler C, Hack A, Korsakov A. 2006. Aqueous fluids and hydrous melts in high-pressure and ultra-high pressure rocks: implications for element transfer in subduction zones. Lithos, 92(3-4): 399~417.
Hilairet N, Reynard B. 2009. Stability and dynamics of serpentinite layer in subduction zone. Tectonophysics, 465(1-4): 24~29.
Hirth G, Guillot S. 2013. Rheology and tectonic significance of serpentinite. Elements, 9(2): 107~113.
Inglis E C. 2017. The behavior of iron and zinc stable isotopes accompanying the subduction of mafic oceanic crust: a case study from Western Alpine ophiolites. Geochemistry, Geophysics, Geosystems, 18(7): 2562~2579.
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 eclogitefacies transport vein in blueschist (Tianshan, China). Lithos, 103(1-2): 1~24.
John T, Scambelluri M, Frische M, Barnes J D, Bach W. 2011. Dehydration of subducting serpentinite: implications for halogen mobility in subduction zones and the deep halogen cycle. Earth and Planetary Science Letters, 308(1-2): 65~76.
Jöns N, Bach W, Klein F. 2010. Magmatic influence on reaction paths and element transport during serpentinization. Chemical Geology, 274(3-4): 196~211.
Kendrick M A, Scambelluri M, Honda M, Phillips D. 2011. High abundances of noble gas and chlorine delivered to the mantle by serpentinite subduction. Nature Geoscience, 4(11): 807~812.
Kendrick M A, Hémond C, Kamenetsky V S, Danyushevsky L, Devey C W, Rodemann T, Jackson M G, Perfit M R. 2017. Seawater cycled throughout Earth's mantle in partially serpentinized lithosphere. Nature Geoscience, 10(3): 222~228.
Kodolányi J, Pettke T, Spandler C, Kamber B S, Gméling K. 2012. Geochemistry of ocean floor and fore-arc serpentinites: constraints on the ultramafic input to subduction zones. Journal of Petrology, 53(2): 235~270.
Lafay R, Deschamps F, Schwartz S, Guillot S, Godard M, Debret B, Nicollet C. 2013. High-pressure serpentinites, a trap-and-release system controlled by metamorphic conditions: example from the Piedmont zone of the western Alps. Chemical Geology, 343: 38~54.
Lazar C, Cooperdock E H G, Seymour B H T. 2021. A continental forearc serpentinite diapir with deep origins: elemental signatures of a mantle wedge protolith and slab-derived fluids at New Idria, California. Lithos, 398: 106252.
Li Xuping, Rahn M, Bucher K. 2004. Serpentinites of the Zermatt-Saas ophiolite complex and their texture evolution. Journal of Metamorphic Geology, 22(3): 159~177.
Li Yuanhui. 1991. Distribution patterns of the elements in the ocean: a synthesis. Geochimica et Cosmochimica Acta, 55(11): 3223~3240.
Li Z X A, Lee C T A. 2006. Geochemical investigation of serpentinized oceanic lithospheric mantle in the Feather River Ophiolite, California: implications for the recycling rate of water by subduction. Chemical Geology, 235(1-2): 161~185.
Liu Shenao, Liu Pingping, Lv Y, Wang Zezhou, Dai Jingen. 2019. Cu and Zn isotope fractionation during oceanic alteration: implications for Oceanic Cu and Zn cycles. Geochimica et Cosmochimica Acta, 257: 191~205.
Malvoisin B. 2015. Mass transfer in the oceanic lithosphere: serpentinization is not isochemical. Earth and Planetary Science Letters, 430: 75~85.
Marchesi C, Garrido C J, Padrón-Navarta J A, López Sánchez-Vizcaíno V, Gómez-Pugnaire M T. 2013. Element mobility from seafloor serpentinization to high-pressure dehydration of antigorite in subducted serpentinite: insights from the Cerro del Almirez ultramafic massif (southern Spain). Lithos, 178: 128~142.
Marschall H R, Schumacher J C. 2012. Arc magmas sourced from mélange diapirs in subduction zones. Nature Geoscience, 5(12): 862~867.
Mellini M, Trommsdorff V, Compagnoni R. 1987. Antigorite polysomatism: behaviour during progressive metamorphism. Contributions to Mineralogy and Petrology, 97(2): 147~155.
Niu Yaoling. 2004. Bulk-rock major and trace element compositions of abyssal peridotites: implications for mantle melting, melt extraction and post-melting processes beneath mid-ocean ridges. Journal of Petrology, 45(12): 2423~2458.
Padrón-Navarta J A, Lopez Sanchez-Vizcaino V, Garrido C J, Gomez-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). Journal of Petrology, 52(10): 2047~2078.
Palme H, O'Neill H St C. 2014. Cosmochemical estimates of mantle composition. Treatise on Geochemistry. Elsevier, 1~39.
Parkinson I J, Pearce J A. 1998. Peridotites from the Izu-Bonin-Mariana Forearc (ODP Leg 125): evidence for mantle melting and melt-mantle interaction in a supra-subduction zone setting. Journal of Petrology, 39(9): 1577~1618.
Paulick H, Bach W, Godard M, De Hoog J C M, Suhr G, Harvey J. 2006. Geochemistry of abyssal peridotites (Mid-Atlantic Ridge, 15°20′N, ODP Leg 209): implications for fluid/rock interaction in slow spreading environments. Chemical Geology, 234(3-4): 179~210.
Pearce J A, Barker P F, Edwards S J, Parkinson I J, Leat P T. 2000. Geochemistry and tectonic significance of peridotites from the south sandwich arc-basin system, South Atlantic. Contributions to Mineralogy and Petrology, 139(1): 36~53.
Perrillat J, Daniel I, Koga K, Reynard B, Cardon H, Crichton W. 2005. Kinetics of antigorite dehydration: a real-time X-ray diffraction study. Earth and Planetary Science Letters, 236(3-4): 899~913.
Peters D, Bretscher A, John T, Scambelluri M, Pettke T. 2017. Fluid-mobile elements in serpentinites: constraints on serpentinisation environments and element cycling in subduction zones. Chemical Geology, 466: 654~666.
Peters D, Pettke T, John T, Scambelluri M. 2020. The role of brucite in water and element cycling during serpentinite subduction—insights from Erro Tobbio (Liguria, Italy). Lithos, 360: 105431.
Pettke T, Bretsche, A. 2022. Fluid-mediated element cycling in subducted oceanic lithosphere: the orogenic serpentinite perspective. Earth-Science Reviews, 225: 103896. Plank T. 2014. The chemical composition of subducting sediments. Treatise on Geochemistry, 4: 607~629.
Plümper O, King H E, Geisler T, Liu Yang, Pabst S, Savov I P, Rost D, Zack T. 2017. Subduction zone forearc serpentinites as incubators for deep microbial life. Proceedings of the National Academy of Sciences, 114(17): 4324~4329.
Pons M L, Quitté G, Fujii T, Rosing M T, Reynard B, Moynier F, Douchet C, Albarède F. 2011. Early Archean serpentine mud volcanoes at Isua, Greenland, as a niche for early life. Proceedings of the National Academy of Sciences, 108(43): 17639~17643.
Pons M L, Debret B, Bouilhol P, Delacour A, Williams H. 2016. Zinc isotope evidence for sulfate-rich fluid transfer across subduction zones. Nature Communications, 7(1): 1~8.
Prichard H M. 1979. A petrographie study of the process of erpentinization in ophiolites and the ocean crust. Contributions to Mineralogy and Petrology, 68(3): 231~241.
Ranero C R, Phipps Morgan J, McIntosh K, Reichert C. 2003. Bending-related faulting and mantle serpentinization at the Middle America trench. Nature, 425(6956): 367~373.
Rebay G, Spalla M I, Zanoni D. 2012. Interaction of deformation and metamorphism during subduction and exhumation of hydrated oceanic mantle: insights from the Western Alps. Journal of Metamorphic Geology, 30(7): 687~702.
Reynard B. 2013. Serpentine in active subduction zones. Lithos, 178: 171~185.
Ribeiro J M, Lee C T A. 2017. An imbalance in the deep water cycle at subduction zones: the potential importance of the fore-arc mantle. Earth and Planetary Science Letters, 479: 298~309.
Rouméjön S, Cannat M, Agrinier P, Godard M, Andreani M. 2015. Serpentinization and fluid pathways in tectonically exhumed peridotites from the southwest Indian ridge (62-65 E). Journal of Petrology, 56(4): 703~734.
Salters V J M, Stracke A. 2004. Composition of the depleted mantle. Geochemistry, Geophysics, Geosystems, 5(5): 1~27.
Saumur B M, Hattori K H, Guillot S. 2010. Contrasting origins of serpentinites in a subduction complex, northern Dominican Republic. Geological Society of America Bulletin, 122(1-2): 292~304.
Savov I P, Guggino S, Ryan J G, Fryer P, Mottl M J. 2005a. Geochemistry of serpentine muds and metamorphic rocks from the Mariana Forearc, ODP Sites 1200 and 778-779, South Chamorro and Conical seamounts. Proceedings of the Ocean Drilling Program, Scientific Results, 195: 1~49.
Savov I P, Ryan J G, D'Antonio M, Kelley K, Mattie P. 2005b. Geochemistry of serpentinized peridotites from the Mariana Forearc conical seamount, ODP leg 125: implications for the elemental recycling at subduction zones. Geochemistry, Geophysics, Geosystems, 6(4): 1~24.
Savov I P, Ryan J G, D'Antonio M, Fryer P. 2007. Shallow slab fluid release across and along the Mariana arc-basin system: insights from geochemistry of serpentinized peridotites from the Mariana fore arc. Journal of Geophysical Research: Solid Earth, 112: B09205.
Scambelluri M, Müntener O, Hermann J, Piccardo G B, Trommsdorff V. 1995. Subduction of water into the mantle: history of an Alpine peridotite. Geology, 23(5): 459~462.
Scambelluri M, Bottazzi P, Trommsdorff V, Vannucci R, Hermann J, GòmezPugnaire M T, Lòpez-Sànchez Vizca1no V. 2001. Incompatible element-rich fluids released by antigorite breakdown in deeply subducted mantle. Earth and Planetary Science Letters, 192(3): 457~470.
Scambelluri M, Tonarini S. 2012. Boron isotope evidence for shallow fluid transfer across subduction zones by serpentinized mantle. Geology, 40(10): 907~910.
Scambelluri M, Pettke T, Rampone E, Godard M, Reusser E. 2014. Petrology and trace element budgets of high-pressure peridotites indicate subduction dehydration of serpentinized mantle(Cima di Gagnone, Central Alps, Switzerland). Journal of Petrology, 55(3): 459~498.
Scambelluri M, Pettke T, Cannaò E. 2015. Fluid-related inclusions in Alpine high-pressure peridotite reveal trace element recycling during subduction-zone dehydration of serpentinized mantle(Cima di Gagnone, Swiss Alps). Earth and Planetary Science Letters, 429: 45~59.
Scambelluri M, Cannaò E, Gilio M. 2019. The water and fluid-mobile element cycles during serpentinite subduction: a review. European Journal of Mineralogy, 31(3): 405~428.
Schwartz S, Allemand P, Guillot S. 2001. Numerical model of the effect of serpentinites on the exhumation of eclogitic rocks: insights from the Monviso ophiolitic massif (western Alps). Tectonophysics, 342(1-2): 193~206.
Schwartz S, Guillot S, Reynard B, Lafay R, Debret B, Nicollet C, Lanari P, Auzende A L. 2013. Pressure-temperature estimates of the lizardite/antigorite transition in high pressure serpentinites. Lithos, 178: 197~210.
Shen Tingting, Hermann J, Zhang Lifei, Padrón-Navarta J A, Chen Jing. 2014. FTIR spectroscopy of Ti-chondrodite, Ti-clinohumite, and olivine in deeply subducted serpentinites and implications for the deep water cycle. Contributions to Mineralogy and Petrology, 167(4): 1~15.
Shen Tingting, Hermann J, Zhang Lifei, Lü Zeng, Padrón-Navarta J A, Xia Bing, Bader T. 2015. UHP metamorphism documented in Ti-chondrodite- and Ti-clinohumite-bearing serpentinized ultramafic rocks from Chinese southwestern Tianshan. Journal of Petrology, 56(7): 1425~1458.
Shen Tingting, Zhang Lifei, Chen Jing. 2016. Metamorphism of subduction zone serpentinite. Acta Petrologica Sinica, 32(4): 1206~1218 (in Chinese with English abstract).
Shen Tingting, Zhang Cong, Chen Jing, Hermann J, Zhang Lifei, Padrón-Navarta J A, Chen Li, Xu Jun, Yang Jingsui. 2020. Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone conditions. American Mineralogist: Journal of Earth and Planetary Materials, 105(4): 569~582.
Sinton J M, Detrick R S. 1992. Mid-ocean ridge magma chambers. Journal of Geophysical Research: Solid Earth, 97(B1): 197~216.
Spandler C, Pirard C. 2013. Element recycling from subducting slabs to arc crust: a review. Lithos, 170: 208~223.
Staub R. 1922. Über die Verteilung der Serpentine in den alpinen Ophiolithen. Schweiz, Verlag nicht ermittelbar, 2: 74~149.
Staudigel H. 2014. Chemical fluxes from hydrothermal alteration of the oceanic crust. In: Holland, H D, Turekian K K, eds. Treatise on Geochemistry(Second Edition). Oxford: Elsevier, 583~603.
Su Benxun, Teng Fangzhen, Hu Yan, Shi Rendeng, Zhou Meifu, Zhu Bin, Liu Fan, Gong Xiaohan, Huang Qishuai, Xiao Yan, Chen Chen, He Yongsheng. 2015. Iron and magnesium isotope fractionation in oceanic lithosphere and sub-arc mantle: perspectives from ophiolites. Earth and Planetary Science Letters, 430: 523~532.
Sun S S, McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications, 42(1): 313~345.
Tatsumi Y. 1986. Formation of the volcanic front in subduction zones. Geophysical Research Letters, 13(8): 717~720.
Tatsumi Y. 2005. The subduction factory: how it operates in the evolving Earth. Gsa Today, 15(7): 4.
Teng Fangzhen, Watkins J M, Dauphas N. 2017. Non-traditional stable isotopes. Reviews in Mineralogy and Geochemistry. Magnesium Isotope Geochemistry, 82: 219~287.
Till C B, Grove T L, Withers A C. 2012. The beginnings of hydrous mantle wedge melting. Contributions to Mineralogy and Petrology, 163(4): 669~688.
Ulmer P, Trommsdorff V. 1995. Serpentine stability to mantle depths and subduction-related magmatism. Science, 268(5212): 858~861.
van Keken P E. 2003. The structure and dynamics of the mantle wedge. Earth and Planetary Science Letters, 215(3-4): 323~338.
Viti C, Mellini M. 1998. Mesh textures and bastites in the Elba retrograde serpentinites. European Journal of Mineralogy, 10(6): 1341~1360.
Whattam S A, Früh-Green G L, Cannat M, De Hoog J C M, Schwarzenbach E M, Escartin J, John B E, Leybourne M I, Williams M J, Rouméjon S, Akizawa N, Boschi C, Harris M, Wenzel K, McCaig A, Weis D, Bilenker L. 2022. Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): petrogenesis and discrimination of melt-rock vs. fluid-rock processes. Chemical Geology, 594: 120681.
Xie Zhipeng, Hattori K, Dong Youpu, Wang Jian. 2021. In situ characterization of forearc serpentinized peridotite from the Sulu ultrahigh-pressure terrane: behavior of fluid-mobile elements in continental subduction zone. Geoscience Frontiers, 12(4): 101139.
Xiong Jiawei, Chen Yixiang, Zhou Kun, Schertl H P, Zheng Yongfei, Huang Fang, Xia Xiaoping, Chen Zhenwu. 2021. Fe and O isotopes in coesite-bearing jadeite quartzite from the Western Alps record multistage fluid-rock interactions in a continental subduction zone. Geochimica et Cosmochimica Acta, 312: 1~24.
Xiong Jiawei, Chen Yixiang, Ma Hezhi, Schertl H P, Zheng Yongfei, Zhao Kuidong. 2022. Tourmaline boron isotopes trace metasomatism by serpentinite-derived fluid in continental subduction zone. Geochimica et Cosmochimica Acta, 320: 122~142.
Zhang Yuxiang, Gazel E, Gaetani G A, Klein F. 2021. Serpentinite-derived slab fluids control the oxidation state of the subarc mantle. Science Advances, 7(48): eabj2515.
Zhao Jing, Long Xiaoping, Li Jie, Zhao Bingshuang, Gao Yilin, Zuo R. 2022. Serpentinite as a tracer for tectonic setting and mantle metasomatism of ophiolites: a case study of the Aoyougou ophiolite in the Qilian Orogenic Belt, NW China. Gondwana Research, 105: 1~11.
Zheng Yongfei. 2019. Subduction zone geochemistry. Geoscience Frontiers, 10(4): 1223~1254.
陈伊翔. 2021. 俯冲带蛇纹岩变质脱水过程中的 Mg, Fe 同位素分馏行为: 进展与展望. 矿物岩石地球化学通报, 40(5): 1034~1048.
申婷婷, 张立飞, 陈晶. 2016. 俯冲带蛇纹岩的变质过程. 岩石学报, 32(4): 1206~1218.