绿帘石记录俯冲带变质流体活动
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摘要
俯冲带是连接地球表生圈层和深部圈层的关键纽带,深刻影响着地球内部的运行方式和人类宜居环境。俯冲板片脱水释放的高压-超高压变质流体控制着俯冲带诸多重要地质过程,如地幔楔交代和部分熔融、岛弧岩浆活动、中/深源地震以及地球内部的元素迁移和分异等等。深入了解这些流体的源区、运移、成分和物理化学条件是理解这些流体性质和行为的前提和关键。绿帘石是俯冲带变质岩中一个常见的含水造岩矿物,具有较宽广的稳定温压范围(绿片岩相-榴辉岩相)、较高的微量元素含量和缓慢的体扩散行为(如Sr、Pb、Th、U、Cr、V和LREE),能够指示俯冲带(多期)变质流体活动和地球化学效应。本文总结了近年来俯冲带变质绿帘石研究的主要进展及其在揭示俯冲带流体活动方面的重要应用,包括探究俯冲带流体的起源、成分特征、运移方式、氧逸度条件、交代效应和多期次结晶行为。这些研究表明绿帘石是一个极好的变质流体活动记录器,能够为理解俯冲带流体活动和深部元素迁移提供关键信息。
Subduction zone is the key link between the earth's surface biosphere and lithosphere,which therefore significantly influences the evolution of the earth interior and habitable environment of human. Suitable scale of mobile fluid phase is commonly present in this setting. Those slab-derived high pressure( HP) or ultra-high pressure( UHP) metamorphic aqueous fluids control the key geological processes in subduction zones,such as the metasomatism and partial melting of mantle wedge,the formation of island arc lavas,the intermediate and deep earthquakes,and the element transfer and chemical differentiation. Knowledge of fluid source,flow manner,composition,and physico-chemical condition is the premise and key to understand the nature and behavior of subduction-zone fluids. Epidote is an important hydrous rock-forming mineral in subduction-zone metamorphic rocks. This mineral has a wide P-T stability range from greenschist facies to eclogite facies,high concentrations of trace elements( e. g.,Sr,Pb,Th,U,Cr,V and LREE),and the negligible in body diffusion,which allow it to reflect the( multiple-stage) fluid activities and geochemical feedbacks in subduction zones. This paper reviewed the main research progress of epidote and its important applications in revealing the subduction-zone fluid activities for the past few years,including the origin,chemical composition,flow manner,oxygen fugacity,metasomatic effect,and multiple-stage crystallization of the fluids. These results indicate that epidote is an excellent recorder of metamorphic fluid actions,which could prove vital information to help understand the metamorphic fluid behavior and element transfer in subduction zones.
Subduction zone is the key link between the earth's surface biosphere and lithosphere,which therefore significantly influences the evolution of the earth interior and habitable environment of human. Suitable scale of mobile fluid phase is commonly present in this setting. Those slab-derived high pressure( HP) or ultra-high pressure( UHP) metamorphic aqueous fluids control the key geological processes in subduction zones,such as the metasomatism and partial melting of mantle wedge,the formation of island arc lavas,the intermediate and deep earthquakes,and the element transfer and chemical differentiation. Knowledge of fluid source,flow manner,composition,and physico-chemical condition is the premise and key to understand the nature and behavior of subduction-zone fluids. Epidote is an important hydrous rock-forming mineral in subduction-zone metamorphic rocks. This mineral has a wide P-T stability range from greenschist facies to eclogite facies,high concentrations of trace elements( e. g.,Sr,Pb,Th,U,Cr,V and LREE),and the negligible in body diffusion,which allow it to reflect the( multiple-stage) fluid activities and geochemical feedbacks in subduction zones. This paper reviewed the main research progress of epidote and its important applications in revealing the subduction-zone fluid activities for the past few years,including the origin,chemical composition,flow manner,oxygen fugacity,metasomatic effect,and multiple-stage crystallization of the fluids. These results indicate that epidote is an excellent recorder of metamorphic fluid actions,which could prove vital information to help understand the metamorphic fluid behavior and element transfer in subduction zones.
引文
Ague JJ and Nicolescu S.2014.Carbon dioxide released from subduction zones by fluid-mediated reactions.Nature Geoscience,7(5):355-360
Andersen T,Austrheim H,Burke EAJ and Elvevold S.1993.N2and CO2in deep crustal fluids:Evidence from the Caledonides of Norway.Chemical Geology,108(1-4):113-132
Angiboust S,Pettke T,De Hoog JCM,Caron B and Oncken O.2014.Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone.Journal of Petrology,55(5):883-916
Arculus RJ.1985.Oxidation status of the mantle:Past and present.Annual Review of Earth and Planetary Sciences,13:75-95
Armbruster T,Bonazzi P,Akasaka M,Bermanec V,Chopin C,GieréR,Heuss-Assbichler S,Liebscher A,Menchetti S,Pan YM and Pasero M.2006.Recommended nomenclature of epidote-group minerals.European Journal of Mineralogy,18(5):551-567
Austrheim H.1987.Eclogitization of lower crustal granulites by fluid migration through shear zones.Earth and Planetary Science Letters,81(2-3):221-232
Bebout GE.2007.Metamorphic chemical geodynamics of subduction zones.Earth and Planetary Science Letters,260(3-4):373-393
Becker H,Jochum KP and Carlson RW.1999.Constraints from highpressure veins in eclogites on the composition of hydrous fluids in subduction zones.Chemical Geology,160(4):291-308
Beinlich A,Klemd R,John T and Gao J.2010.Trace-element mobilization during Ca-metasomatism along a major fluid conduit:Eclogitization of blueschist as a consequence of fluid-rock interaction.Geochimica et Cosmochimica Acta,74(6):1892-1922
Bermanec V,Armbruster T,Oberhnsli R and Zebec V.1994.Crystal chemistry of Pb-and REE-rich piemontite from Nezilovo,Macedonia.Schweizerische Mineralogische und Petrographische Mitteilungen,74:321-328
Bieseler B,Diehl A,J9ns N,Lucassen F and Bach W.2018.Constraints on cooling of the lower ocean crust from Epidote veins in the Wadi Gideah Section,Oman ophiolite.Geochemistry,Geophysics,Geosystems,19(11):4195-4217
Bonazzi P and Menchetti S.2004.Manganese in monoclinic members of the epidote group:Piemontite and related minerals.Reviews in Mineralogy and Geochemistry,56(1):495-552
Brastad K.1985.Sr metasomatism,and partition of Sr between the mineral phases of a meta-eclogite from Bjrkedalen,West Norway.Tschermaks Mineralogische und Petrographische Mitteilungen,34(2):87-103
Brenan JM,Ryerson FJ and Shaw HF.1998.The role of aqueous fluids in the slab-to-mantle transfer of boron,beryllium,and lithium during subduction:Experiments and models.Geochimica et Cosmochimica Acta,62(19-20):3337-3347
Brovarone AV and Beyssac O.2014.Lawsonite metasomatism:A new route for water to the deep earth.Earth and Planetary Science Letters,393:275-284
Brovarone AV,Chu X,Martin L,Ague JJ,MoniéP,Groppo C,Martinez I and Chaduteau C.2018.Intra-slab COH fluid fluxes evidenced by fluid-mediated decarbonation of lawsonite eclogitefacies altered oceanic metabasalts.Lithos,304-307:211-229
Brunsmann A,Franz G,Erzinger J and Landwehr D.2000.Zoisite-and clinozoisite-segregations in metabasites(Tauern Window,Austria)as evidence for high-pressure fluid-rock interaction.Journal of Metamorphic Geology,18(1):1-21
Brunsmann A,Franz G and Erzinger J.2001.REE mobilization during small-scale high-pressure fluid-rock interaction and zoisite/fluid partitioning of La to Eu.Geochimica et Cosmochimica Acta,65(4):559-570
Brunsmann A,Franz G and Heinrich W.2002.Experimental investigation of zoisite-clinozoisite phase equilibria in the system CaO-Fe2O3-Al2O3-SiO 2-H2O.Contributions to Mineralogy and Petrology,143(1):115-130
Campos-Alvarez NO,Samson IM,Fryer BJ and Ames DE.2010.Fluid sources and hydrothermal architecture of the Sudbury Structure:Constraints from femtosecond LA-MC-ICP-MS Sr isotopic analysis of hydrothermal epidote and calcite.Chemical Geology,278(3-4):131-150
Cao MJ,Qin KZ,Li GM,Evans NJ,McI nnes BIA,Li JX and Zhao JX.2018.Oxidation state inherited from the magma source and implications for mineralization:Late Jurassic to Early Cretaceous granitoids,Central Lhasa subterrane,Tibet.Mineralium Deposita,53(3):299-309
Cao Y,Song SG,Niu YL,Jung H and Jin ZM.2011.Variation of mineral composition,fabric and oxygen fugacity from massive to foliated eclogites during exhumation of subducted ocean crust in the North Qilian suture zone,NW China.Journal of Metamorphic Geology,29(7):699-720
Castelli D,Rolfo F,Compagnoni R and Xu ST.1998.Metamorphic veins with kyanite,zoisite and quartz in the Zhujiachong eclogite,Dabie Shan,China.Island Arc,7(1-2):159-173
Chen RX,Zheng YF and Hu ZC.2012.Episodic fluid action during exhumation of deeply subducted continental crust:Geochemical constraints from zoisite-quartz vein and host metabasite in the Dabie orogen.Lithos,155:146-166
Chen YX,Zheng YF,Gao XY and Hu ZC.2014.Multiphase solid inclusions in zoisite-bearing eclogite:Evidence for partial melting of ultrahigh-pressure metamorphic rocks during continental collision.Lithos,200-201:1-21
Choo CO.2002.Complex compositional zoning in epidote from rhyodacitic tuff,Bobae sericite deposit,Southeastern Korea.Journal of Mineralogy and Geochemistry,177(2):181-197
Clarke GL,Powell R and Fitzherbert JA.2006.The lawsonite paradox:A comparison of field evidence and mineral equilibria modelling.Journal of Metamorphic Geology,24(8):715-725
Davies JH.1999.The role of hydraulic fractures and intermediate-depth earthquakes in generating subduction-zone magmatism.Nature,398(6723):142-145
Davis PB and Whitney DL.2006.Petrogenesis of lawsonite and epidote eclogite and blueschist,Sivrihisar Massif,Turkey.Journal of Metamorphic Geology,24(9):823-849
Deer WA,Howie RA and Zussman J.1986.Rock-Forming Minerals,Vol 1B,Disilicates and Ring Silicates.2ndEdition.New York:Longman,1-629
Donohue CL and Essene EJ.2000.An oxygen barometer with the assemblage garnet-epidote.Earth and Planetary Science Letters,181(3):459-472
Eide EA and Liou JG.2000.High-pressure blueschists and eclogites in Hong’an:A framework for addressing the evolution of high-and ultrahigh-pressure rocks in central China.Lithos,52(1-4):1-22
El Korh A,Schmidt ST,Ulianov A and Potel S.2009.Trace element partitioning in HP-LT metamorphic assemblages during subductionrelated metamorphism,Ile de Groix,France:A detailed LA-ICPMSstudy.Journal of Petrology,50(6):1107-1148
Enami M,Liou JG and Mattinson CG.2004.Epidote minerals in high P/T metamorphic terranes:Subduction zone and high-to ultrahighpressure metamorphism.Reviews in Mineralogy and Geochemistry,56(1):347-398
Eskola PE.1933.On the chrome minerals of Outokumpu.Bulletin de la Comission Gèologique de Finlande,103:26-44
Feineman MD,Ryerson FJ,DeP aolo DJ and Plank T.2007.Zoisiteaqueous fluid trace element partitioning with implications for subduction zone fluid composition.Chemical Geology,239(3-4):250-265
Finger F,Broska I,Roberts MP and Schermaier A.1998.Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps.AmericanMineralogist,83(3-4):248-258
Frank MR,Candela PA,Piccoli PM and Glascock MD.2002.Gold solubility,speciation,and partitioning as a function of HCL in the brine-silicate melt-metallic gold system at 800℃and 100MPa.Geochimica et Cosmochimica Acta,66(21):3719-3732
Franz G and Liebscher A.2004.Physical and chemical properties of the epidote minerals:An introduction.Reviews in Mineralogy and Geochemistry,56(1):1-81
Franz L,Romer RL,Klemd R,Schimd R,Oberhnsli R,Wagner T and Dong SW.2001.Eclogite-facies quartz veins within metabasites of the Dabie Shan(eastern China):Pressure-temperature-timedeformation path,composition of the fluid phase and fluid flow during exhumation of high-pressure rocks.Contributions to Mineralogy and Petrology,141(3):322-346
Frei D,Liebscher A,Franz G and Dulski P.2004.Trace element geochemistry of epidote minerals.Reviews in Mineralogy and Geochemistry,56(1):553-605
Fu B,Touret JLR and Zheng YF.2001.Fluid inclusions in coesitebearing eclogites and jadeite quartzite at Shuanghe,Dabie Shan(China).Journal Metamorphic Geology,19(5):531-547
Gao J and Klemd R.2001.Primary fluids entrapped at blueschist to eclogite transition:Evidence from the Tianshan meta-subduction complex in northwestern China.Contributions to Mineralogy and Petrology,142(1):1-14
Gao J,John T,Klemd R and Xiong XM.2007.Mobilization of Ti-Nb-Ta during subduction:Evidence from rutile-bearing dehydration segregations and veins hosted in eclogite,Tianshan,NW China.Geochimica et Cosmochimica Acta,71(20):4974-4996
Gao XY,Zheng YF and Chen YX.2012.Dehydration melting of ultrahigh-pressure eclogite in the Dabie orogen:Evidence from multiphase solid inclusions in garnet.Journal of Metamorphic Geology,30(2):193-212
Gatta GD,Merlini M,Lee Y and Poli S.2011.Behavior of epidote at high pressure and high temperature:A powder diffraction study up to10GPa and 1,200K.Physics and Chemistry of Minerals,38(6):419-428
GieréR and Sorensen SS.2004.Allanite and other REE-rich epidotegroup minerals.Reviews in Mineralogy and Geochemistry,56(1):431-493
Gottschalk M.2004.Thermodynamic properties of zoisite,clinozoisite and epidote.Reviews in Mineralogy and Geochemistry,56(1):83-124
Grapes RH.1981.Chromian epidote and zoisite in kyanite amphibolite,Southern Alps,New Zealand.American Mineralogist,66:974-975
Grapes RH and Watanabe T.1984.Al-Fe3+and Ca-Sr2+epidotes in metagreywacke-quartzofeldspathic schist,Southern Alps,New Zealand.American Mineralogist,69:490-498
Grapes RH and Hoskin PWO.2004.Epidote group minerals in lowmedium pressure metamorphic terranes.Reviews in Mineralogy and Geochemistry,56(1):301-345
Guo HH,Xiao YL,Xu LJ,Sun H,Huang J and Hou ZH.2017a.Origin of allanite in gneiss and granite in the Dabie orogenic belt,Central East China.Journal of Asian Earth Sciences,135:243-256
Guo S,Ye K,Chen Y,Liu JB,Mao Q and Ma YG.2012.Fluid-rock interaction and element mobilization in UHP metabasalt:Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen.Lithos,136-139:145-167
Guo S,Ye K,Wu TF,Chen Y,Yang YH,Zhang LM,Liu JB,Mao Qand Ma YG.2013.A potential method to confirm the previous existence of lawsonite in eclogite:The mass imbalance of Sr and LREEs in multistage epidote(Ganghe,Dabie UHP terrane).Journal of Metamorphic Geology,31(4):415-435
Guo S,Ye K,Yang YH,Chen Y,Zhang LM,Liu JB,Mao Q and Ma YG.2014.In situ Sr isotopic analyses of epidote:Tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite(Ganghe,Dabie terrane).Contributions to Mineralogy and Petrology,167(2):975
Guo S,Chen Y,Ye K,Su B,Yang YH,Zhang LM,Liu JB and Mao Q.2015a.Formation of multiple high-pressure veins in ultrahighpressure eclogite(Hualiangting,Dabie terrane,China):Fluid source,element transfer,and closed-system metamorphic veining.Chemical Geology,417:238-260
Guo S,Ye K,Cheng NF,Chen Y,Su B and Liu JB.2015b.Metamorphic P-T trajectory and multi-stage fluid events of veinbearing UHP eclogites from the Dabie terrane:Insights from compositional zonations of key minerals.International Geology Review,57(9-10):1077-1102
Guo S,Yang YH,Chen Y,Su B,Gao YJ,Zhang LM,Liu JB and Mao Q.2016.Grainscale Sr isotope heterogeneity in amphibolite(retrograded UHP eclogite,Dabie terrane):Implications for the origin and flow behavior of retrograde fluids during slab exhumation.Lithos,266-267:383-405
Guo S,Tang P,Su B,Chen Y,Ye K,Zhang LM,Gao YJ,Liu JB and Yang YH.2017b.Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins(Dabie UHPterrane):A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs.American Mineralogist,102(11):2268-2283
Guo S,Zhao KD,John T,Tang P,Chen Y and Su B.2019.Metasomatic flow of metacarbonate-derived fluids carrying isotopically heavy boron in continental subduction zones:Insights from tourmaline-bearing ultra-high pressure eclogites and veins(Dabie terrane,eastern China).Geochimica et Cosmochimica Acta,253:159-200
Hacker BR,Peacock SM,Abers GA and Holloway SD.2003.Subduction factory 2.Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions?Journal of Geophysical Research,108(B1):2030
Harris C,Hlongwane W,Gule N and Scheepers R.2014.Origin of tanzanite and associated gemstone mineralization at Merelani,Tanzania.South African Journal of Geology,117(1):15-30
Haüy RJ.1801.Traitéde Minérologie.Chez Louis Libraire,Paris,102-113
Hermann J.2002.Allanite:Thorium and light rare earth element carrier in subducted crust.Chemical Geology,192(3-4):289-306
Hermann J,Spandler C,Hack A and Korsakov AV.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
Hirajima T,Zhang R,Li J and Cong B.1992.Petrology of the nyb9itebearing eclogite in the Donghai area,Jiangsu Province,eastern China.Mineralogical Magazine,56(382):37-46
Holdaway MJ.1972.Thermal stability of AI-Fe epidote as a function of fOand Fe content.Contributions to Mineralogy and Petrology2,37(4):307-340
Hu HY,Dai LD,Li HP,Hui KS and Sun WQ.2017.Influence of dehydration on the electrical conductivity of epidote and implications for high-conductivity anomalies in subduction zones.Journal of Geophysical Research:Solid Earth,122:2751-2762
Huang J,Xiao Y,Gao Y,Hou Z and Wu W.2012.Nb-Ta fractionation induced by fluid-rock interaction in subduction-zones:Constraints from UHP eclogite-and vein-hosted rutile from the Dabie orogen,Central-Eastern China.Journal of Metamorphic Geology,30(8):821-842
Jan cˇev S and Bermanec V.1998.Solid solution between epidote and hancockite from Nezilovo,Macedonia.Geologia Croatica,51(1):23-26
John T,Scherer EE,Haase KM and Schenk V.2004.Trace element fractionation during fluid-induced eclogitization in a subducting slab:Trace element and Lu-Hf-Sm-Nd isotope systematics.Earth and Planetary Science Letters,227(3-4):441-456
John T,Klemd R,Gao J and Garbe-Sch9nberg CD.2008.Trace-element mobilization in slabs due to non steady-state fluid-rock interaction:Constraints from an eclogite-facies transport vein in blueschist(Tianshan,China).Lithos,103(1-2):1-24
John T,Gussone N,Podladchikov YY,Bebout GE,Dohmen R,Halama R,Klemd R,Magna T and Seitz HM.2012.Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs.Nature Geoscience,5(7):489-492
Klemd R.2004.Fluid inclusions in epidote minerals and fluid development in epidote-bearing rocks.Reviews in Mineralogy and Geochemistry,56(1):197-234
Klemd R.2012.Metasomatism during high-pressure metamorphism:Eclogites and blueschist-facies rocks.In:Harlov DE and Austrheim H(eds.).Metasomatism and the Chemical Transformation of Rock:The Role of Fluids in Terrestrial and Extraterrestrial Processes.Berlin Heidelberg:Springer-Verlag,351-413
Korsakov AV and Hermann J.2006.Silicate and carbonate melt inclusions associated with diamonds in deeply subducted carbonate rocks.Earth and Planetary Science Letters,241(1-2):104-118
Li JL,Gao J,John T,Klemd R and Su W.2013.Fluid-mediated metal transport in subduction zones and its link to arc-related giant ore deposits:Constraints from a sulfide-bearing HP vein in lawsonite eclogite(Tianshan,China).Geochimica et Cosmochimica Acta,120:326-362
Li XP,Zheng YF,Wu YB,Chen FK,Gong B and Li YL.2004.Low-Teclogite in the Dabie terrane of China:Petrological and isotopic constraints on fluid activity and radiometric dating.Contributions to Mineralogy and Petrology,148(4):443-470
Li YL,Zheng YF,Fu B,Zhou JB and Wei CS.2001.Oxygen isotope composition of quartz-vein in ultrahigh-pressure eclogite from Dabieshan and implications for transport of high-pressure metamorphic fluid.Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,26(9-10):695-704
Liang JL,Sun XM,Xu L,Zhai W,Tang Q and Liang YH.2006.Geochemistry of epidotes in HP-UHP metamorphic rocks from Chinese Continental Scientific Drilling(CCSD)Project and Qinglongshan area:An indicator of partial melting during continental slab exhumation.Acta Petrologica Sinica,22(7):1845-1854(in Chinese with English abstract)
Liou JG.1973.Synthesis and stability relations of epidote,Ca2Al2FeS i3O12(OH).Journal of Petrology,14(3):381-413
Liou JG,Kim HS and Maruyama S.1983.Prehnite-epidote equilibria and their petrologic applications.Journal of Petrology,24(4):321-342
Liu FL,Gerdes A,Liou JG,Xue HM and Liang FH.2006.SHRIMP U-Pb zircon dating from Sulu-Dabie dolomitic marble,eastern China:Constraints on prograde,ultrahigh-pressure and retrograde metamorphic ages.Journal of Metamorphic Geology,24(7):569-589
Liu PL,Wu Y,Chen Y,Zhang JF and Jin ZM.2015.UHP impure marbles from the Dabie Mountains:Metamorphic evolution and carbon cycling in continental subduction zones.Lithos,212-215:280-297
Liu PL,Zhang JF,Massonne HJ and Jin ZM.2018.Polyphase solidinclusions formed by interactions between infiltrating fluids and precursor minerals enclosed in garnet of UHP rocks from the Dabie Shan,China.American Mineralogist,103(10):1663-1673
Liu XC,Dong SW,Xue HM and Zhou JX.1999.Significance of allanite-(Ce)in granitic gneisses from the ultrahigh-pressure metamorphic terrane,Dabie Shan,central China.Mineralogical Magazine,63(4):579-586
Liu XC,Jahn BM,Dong SW,Li HM and Oberhnsli R.2003.Neoproterozoic granitoid did not record ultrahigh-pressure metamorphism from the southern Dabieshan of China.The Journal of Geology,111(6):719-732
Malisa EPJ.2003.Trace elements characterization of the hydrothermally deposited tanzanite and green grossular in the Merelani-Lelatema shear zone,northeastern Tanzania.Tanzania Journal of Science,29(1):45-60
Manning CE.2004.The chemistry of subduction-zone fluids.Earth and Planetary Science Letters,223(1-2):1-16
Martin LAJ,Wood BJ,Turner S and Rushmer T.2011.Experimentalmeasurements of trace element partitioning between lawsonite,zoisite and fluid and their implication for the composition of arc magmas.Journal of Petrology,52(6):1049-1075
Massonne HJ and O’Brien PJ.2003.The Bohemian massif and the NWHimalaya.In:Carswell DA,Compagnoni R and Rolfo F(eds.).Ultrahigh Pressure Metamorphism.European Mineralogical Union Notes in Mineralogy,5:145-188
Massonne HJ.2012.Formation of amphibole and clinozoisite-epidote in eclogite owing to fluid infiltration during exhumation in a subduction channel.Journal of Petrology,53(10):1969-1998
Mattinson CG,Zhang RY,Tsujimori T and Liou JG.2004.Epidote-rich talc-kyanite-phengite eclogites,Sulu terrane,eastern China:P-T-fOestimates and the significance of the epidote-talc assemblage in2eclogite.American Mineralogist,89(11-12):1772-1783
McC ulloch MT and Gamble JA.1991.Geochemical and geodynamical constraints on subduction zone magmatism.Earth and Planetary Science Letters,102(3-4):358-374
Mengason MJ,Candela PA and Piccoli PM.2011.Molybdenum,tungsten and manganese partitioning in the system pyrrhotite-Fe-S-Omelt-rhyolite melt:Impact of sulfide segregation on arc magma evolution.Geochimica et Cosmochimica Acta,75(22):7018-7030
Miyajima H,Matsubara S,Miyawaki R and Hirokawa K.2003.Niigataite,CaSrAl3(Si2O7)(SiO 4)O(OH):Sr-analogue of clinozoisite,a new member of the epidote group from the ItoigawaOhmi district,Niigata Prefecture,central Japan.Journal of Mineralogical and Petrological Sciences,98(3):118-129
Miyashiro A and Seki Y.1958.Enlargement of the composition field of epidote and piemontite with rising temperature.American Journal of Science,256(6):423-430
Mungall JE.2002.Roasting the mantle:Slab melting and the genesis of major Au and Au-rich Cu deposits.Geology,30(10):915-918
Nagasaki A and Enami M.1998.Sr-bearing zoisite and epidote in ultrahigh pressure(UHP)metamorphic rocks from the Su-Lu provinces,eastern China:An important Sr reservoir under UHP conditions.American Mineralogist,83(3-4):240-247
Nagashima M,Akasaka M and Sakurai T.2006.Chromian epidote in omphacite rocks from the Sambagawa metamorphic belt,central Shikoku,Japan.Journal of Mineralogical and Petrological Sciences,101(4):157-169
Nagashima M,Nishio-Hamane D,Nakano N and Kawasaki T.2019.Synthesis and crystal chemistry of mukhinite,V-analogue of clinozoisite on the join Ca2Al3Si3O12(OH)-Ca2Al2VSi3O12(OH).Physics and Chemistry of Minerals,46(1):63-76
Naney MT.1983.Phase equilibria of rock-forming ferromagnesian silicates in granitic systems.American Journal of Science,283(10):993-1033
Ni HW,Zheng YF,Mao Z,Wang Q,Chen RX and Zhang L.2017.Distribution,cycling and impact of water in the Earth’s interior.National Science Review,4(6):879-891
Oh CW,Liou JG and Maruyama S.1991.Low-temperature eclogites and eclogitic schists in Mn-rich metabasites in Ward Creek,California:Mn and Fe effects on the transition between blueschist and eclogite.Journal of Petrology,32(2):275-302
Pawley AR.1994.The pressure and temperature stability limits of lawsonite:Implications for H2O recycling in subduction zones.Contributions to Mineralogy and Petrology,118(1):99-108
Peacock SA.1990.Fluid processes in subduction zones.Science,248(4953):329-337
Poli S and Schmidt MW.1995.H2O transport and release in subduction zones:Experimental constraints on basaltic and andesitic systems.Journal of Geophysical Research:Solid Earth,100(B11):22299-22314
Poli S and Schmidt MW.1998.The high-pressure stability of zoisite and phase relationships of zoisite-bearing assemblages.Contributions to Mineralogy and Petrology,130(2):162-175
Poli S and Schmidt MW.2004.Experimental subsolidus studies on epidote minerals.Epidotes.Reviews in Mineralogy andGeochemistry,56(1):171-195
Poli S.2016.Melting carbonated epidote eclogites:Carbonatites from subducting slabs.Progress in Earth and Planetary Science,3:27
Potel S,Schmidt ST and de Capitani C.2002.Composition of pumpellyite,epidote and chlorite from New Caledonia:How important are metamorphic grade and whole-rock composition?Schweizerische Mineralogische und Petrographische Mitteilungen,82(1):229-252
Rolfo F,Compagnoni R,Xu ST and Jiang LL.2000.First report of felsic whiteschist in the ultrahigh-pressure metamorphic belt of Dabie Shan,China.European Journal of Mineralogy,12(4):883-898
Romer RL and Xiao YL.2005.Initial Pb-Sr(-Nd)isotopic heterogeneity in a single allanite-epidote crystal:Implications of reaction history for the dating of minerals with low parent-to-daughter ratios.Contributions to Mineralogy and Petrology,148(6):662-674
Rubatto D,Williams IS and Buick IS.2001.Zircon and monazite response to prograde metamorphism in the Reynolds Range,central Australia.Contributions to Mineralogy and Petrology,140(4):458-468
Rubatto D and Hermann J.2003.Zircon formation during fluid circulation in eclogites(Monviso,Western Alps):Implications for Zr and Hf budget in subduction zones.Geochimica et Cosmochimica Acta,67(12):2173-2187
Rubatto D and Angiboust S.2015.Oxygen isotope record of oceanic and high-pressure metasomatism:A P-T-time-fluid path for the Monviso eclogites(Italy).Contributions to Mineralogy and Petrology,170(5-6):44
Santosh M,Tsunogae T,Shimizu H and Dubessy J.2010.Fluid characteristics of retrogressed eclogites and mafic granulites from the Cambrian Gondwana suture zone in southern India.Contributions to Mineralogy and Petrology,159(3):349-369
Sassi R,Harte B,Carswell DA and Yujing H.2000.Trace element distribution in Central Dabie eclogites.Contributions to Mineralogy and Petrology,139(3):298-315
Scambelluri M and Philippot P.2001.Deep fluids in subduction zones.Lithos,55(1-4):213-227
Schmidt MW and Poli S.1994.The stability of lawsonite and zoisite at high pressures:Experiments in CASH to 92kbar and implications for the presence of hydrous phases in subducted lithosphere.Earth and Planetary Science Letters,124(1-4):105-118
Schmidt MW and Thompson AB.1996.Epidote in calc-alkaline magmas:An experimental study of stability,phase relationships,and the role of epidote in magmatic evolution.American Mineralogist,81(3-4):462-474
Schmidt MW and Poli S.1998.Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation.Earth and Planetary Science Letters,163(1-4):361-379
Sheng YM,Zheng YF,Chen RX,Li QL and Dai MN.2012.Fluid action on zircon growth and recrystallization during quartz veining within UHP eclogite:Insights from U-Pb ages,O-Hf isotopes and trace elements.Lithos,136-139:126-144
Skjerlie KP and Pati1o Douce AE.2002.The fluid-absent partial melting of a zoisite-bearing quartz eclogite from 1.0 to 3.2GPa:Implications for melting in thickened continental crust and for subduction-zone processes.Journal of Petrology,43(2):291-314
Sobolev NV and Shatsky VS.1990.Diamond inclusions in garnets from metamorphic rocks:A new environment for diamond formation.Nature,343(6260):742-746
Song SG,Niu YL,Su L,Wei CJ and Zhang LF.2014.Adakitic(tonalitic-trondhjemitic)magmas resulting from eclogite decompression and dehydration melting during exhumation in response to continental collision.Geochimica et Cosmochimica Acta,130:42-62
Sorensen SS and Grossman JN.1989.Enrichment of trace elements in garnet amphibolites from a paleo-subduction zone:Catalina Schist,southern California.Geochimica et Cosmochimica Acta,53(12):3155-3177
Spandler C,Hermann J,Arculus R and Mavrogenes J.2003.Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies:Implications for deep subduction-zone processes.Contributions to Mineralogy and Petrology,146(2):205-222
Spandler C,Pettke T and 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.Journal of Petrology,52(6):1207-1236
Spiegel C,Siebel W,Frisch W and Berner Z.2002.Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators:Implications for the reconstruction of the exhumation history of the Central Alps.Chemical Geology,189(3-4):231-250
Sun WD,Arculus RJ,Kamenetsky VS and Binns RA.2004.Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization.Nature,431(7011):975-978
Svensen H,Jamtveit B,Banks DA and Austrheim H.2001.Halogen contents of eclogite facies fluid inclusions and minerals:Caledonides,western Norway.Journal of Metamorphic Geology,19(2):165-178
Tatsumi Y and Eggins S.1995.Subduction Zone Magmatism.Cambridge,MA:Blackwell Science
Teyssier C,Whitney DL,Toraman E and Seaton NCA.2010.Lawsonite vorticity and subduction kinematics.Geology,38(12):1123-1126
Treloar PJ.1987a.Chromian muscovites and epidotes from Outokumpu,Finland.Mineralogical Magazine,51(62):593-599
Treloar PJ.1987b.The Cr-minerals of Outokumpu:Their chemistry and significance.Journal of Petrology,28(5):867-886
Tumiati S,Godard G,Martin S,Nimis P,Mair V and Boyer B.2005.Dissakisite-(La)from the Ulten zone peridotite(Italian Eastern Alps):A new end-member of the epidote group.American Mineralogist,90(7):1177-1185
Uher P,Kovácˇik M,Kubi2 M,Shtukenberg A and Ozd'n D.2008.Metamorphic vanadian-chromian silicate mineralization in carbon-rich amphibole schists from the MaléKarpaty Mountains,Western Carpathians,Slovakia.American Mineralogist,93(1):63-73
van der Straaten F,Schenk V,John T and Gao J.2008.Blueschistfacies rehydration of eclogites(Tian Shan,NW-China):Implications for fluid-rock interaction in the subduction channel.Chemical Geology,255(1-2):195-219
Verlaguet A,GofféB,Brunet F,Poinssot C,Vidal O,Findling N and Menut D.2011.Metamorphic veining and mass transfer in a chemically closed system:A case study in Alpine metabauxites(western Vanoise).Journal of Metamorphic Geology,29(3):275-300
Volkova NI,Frenkel AE,Budanov VI and Lepezin GG.2004.Geochemical signatures for eclogite protolith from the Maksyutov Complex,South Urals.Journal of Asian Earth Sciences,23(5):745-759
Vrijmoed JC,Austrheim H,John T,Hin RC,Corfu F and Davies GR.2013.Metasomatism in the ultrahigh-pressure Svartberget garnetsperidotite(Western Gneiss Region,Norway):Implications for the transport of crust-derived fluids within the mantle.Journal of Petrology,54(9):1815-1848
Wang SJ,Wang L,Brown M,Piccoli PM,Johnson TE,Feng P,Deng H,Kitajima K and Huang Y.2017.Fluid generation and evolution during exhumation of deeply subducted UHP continental crust:Petrogenesis of composite granite-quartz veins in the Sulu belt,China.Journal of Metamorphic Geology,35(6):601-629
Watenphul A,Schmidt C and Jahn S.2014.Cr(Ⅲ)solubility in aqueous fluids at high pressures and temperatures.Geochimica et Cosmochimica Acta,126:212-227
Wei CJ,Li YJ,Yu Y and Zhang JS.2010.Phase equilibria and metamorphic evolution of glaucophane-bearing UHP eclogites from the Western Dabieshan Terrane,Central China.Journal of Metamorphic Geology,28(6):647-666
Wei CJ and Clarke GL.2011.Calculated phase equilibria for MORBcompositions:A reappraisal of the metamorphic evolution oflawsonite eclogite.Journal of Metamorphic Geology,29(9):939-952
Wei CJ and Cui Y.2011.Metamorphic evolution during subduction and exhumation of crust:Evidence from phase equilibria modelling for high-and ultrahigh-pressure eclogites.Acta Petrologica Sinica,27(4):1067-1074(in Chinese with English abstract)
Whitney DL and Davis PB.2006.Why is lawsonite eclogite so rare?Metamorphism and preservation of lawsonite eclogite,Sivrihisar,Turkey.Geology,34(6):473-476
Whitney DL and Evans BW.2010.Abbreviations for names of rockforming minerals.American Mineralogist,95(1):185-187
Wu YB,Gao S,Zhang HF,Yang SH,Liu XC,Jiao WF,Liu YS,Yuan HL,Gong HJ and He MC.2009.U-Pb age,trace-element,and Hfisotope compositions of zircon in a quartz vein from eclogite in the western Dabie Mountains:Constraints on fluid flow during early exhumation of ultrahigh-pressure rocks.American Mineralogist,94(2-3):303-312
Xia QK,Liu J,Kovács I,Hao YT,Li P,Yang XZ,Chen H and Sheng YM.2019.Water in the upper mantle and deep crust of eastern China:Concentration,distribution and implications.National Science Review,6(1):125-144
Xiao YL,Hoefs J,van den Kerkhof AM,Fiebig J and Zheng YF.2000.Fluid history of UHP metamorphism in Dabie Shan,China:A fluid inclusion and oxygen isotope study on the coesite-bearing eclogite from Bixiling.Contributions to Mineralogy and Petrology,139(1):1-16
Xiao YL,Hoefs J,Hou ZH,Simon K and Zhang ZM.2011.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.Contributions to Mineralogy and Petrology,162(4):797-819
Xiao YL,Sun H,Gu HO,Huang J,Li WY and Liu L.2015.Fluid/melt in continental deep subduction zones:Compositions and related geochemical fractionations.Science China(Earth Sciences),58(9):1457-1476
Xiao YL,Yu CL,Wand YY and Lu YG.2018.Metamorphism and fluid inclusions:An overview and prospectives.Bulletin of Mineralogy,Petrology and Geochemistry,37(3):424-440(in Chinese with English abstract)
Yang JJ and Enami M.2003.Chromian dissakisite-(Ce)in a garnet lherzolite from the Chinese Su-Lu UHP metamorphic terrane:Implications for Cr incorporation in epidote-group minerals and recycling of REE into the Earth’s mantle.American Mineralogist,88(4):604-610
Yao YP,Ye K,Liu JB,Cong BL and Wang QC.2000.A transitional eclogite-to high pressure granulite-facies overprint on coesite-eclogite at Taohang in the Sulu ultrahigh-pressure terrane,eastern China.Lithos,52(1-4):109-120
Zack T,Rivers T,Brumm R and Kronz A.2004.Cold subduction of oceanic crust:Implications from a lawsonite eclogite from the Dominican Republic.European Journal of Mineralogy,16(6):909-916
Zhai W,Sun XM,Liang JL,Xu L,Tang Q,Liang YH and Su LW.2006.Chemical compositions and fluid inclusions of epidotes in Qinglongshan ultrahigh pressure metamorphic eclogite,North Jiangsu Province,China.Acta Petrologica Sinica,22(7):2029-2038(in Chinese with English abstract)
Zhang HF,Gao S,Zhong ZQ,Zhang BR,Zhang L and Hu SH.2002.Geochemical and Sr-Nd-Pb isotopic compositions of Cretaceous granitoids:Constraints on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt,China.Chemical Geology,186(3-4):281-299
Zhang RY.1992.Petrogenesis of high pressure metamorphic rocks in the Su-Lu and Dianxi regions,China.Ph.D.Dissertation.Kyoto:Kyoto University,1-176
Zhang RY,Hirajima T,Banno S,Cong B and Liou JG.1995.Petrology of ultrahigh-pressure rocks from the southern Su-Lu region,EasternChina.Journal of Metamorphic Geology,13(6):659-675
Zhang RY,Liou JG,Ernst WG,Coleman RG,Sobolev NV and Shatsky VS.1997.Metamorphic evolution of diamond-bearing and associated rocks from the Kokchetav Massif,northern Kazakhstan.Journal of Metamorphic Geology,15(4):479-496
Zhang ZM,Xiao YL,Liu FL,Liou JG and Hoefs J.2005.Petrogenesis of UHP metamorphic rocks from Qinglongshan,southern Sulu,eastcentral China.Lithos,81(1-4):189-207
Zhang ZM,Zhang JF,You ZD and Sheng K.2005.Ultrahigh-pressure metamorphic P-T-t path of the Sulu orogenic belt,eastern central China.Acta Petrologica Sinica,21(2):257-270(in Chinese with English abstract)
Zhang ZM,Shen K,Sun WD,Liu YS,Liou JG,Shi C and Wang JL.2008.Fluids in deeply subducted continental crust:Petrology,mineral chemistry and fluid inclusion of UHP metamorphic veins from the Sulu orogen,eastern China.Geochimica et Cosmochimica Acta,72(13):3200-3228
Zhang ZM and Shen K.2009.Fluids from the deeply continental subduction zone and the metamorphic chemical geodynamics.Acta Geoscientia Sinica,30(1):5-20(in Chinese with English abstract)
Zhao YJ,Wu YB,Liu XC,Gao S,Wang H,Zheng JP and Yang SH.2016.Distinct zircon U-Pb and O-Hf-Nd-Sr isotopic behaviour during fluid flow in UHP metamorphic rocks:Evidence from metamorphic veins and their host eclogite in the Sulu Orogen,China.Journal of Metamorphic Geology,34(4):343-362
Zheng YF,Gao TS,Wu YB,Gong B and Liu XM.2007.Fluid flow during exhumation of deeply subducted continental crust:Zircon U-Pb age and O-isotope studies of a quartz vein within ultrahighpressure eclogite.Journal of Metamorphic Geology,25(2):267-283
Zheng YF.2009.Fluid regime in continental subduction zones:Petrological insights from ultrahigh-pressure metamorphic rocks.Journal of the Geological Society,166(4):763-782
Zheng YF,Xia QX,Chen RX and Gao XY.2011.Partial melting,fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision.Earth-Science Reviews,107(3-4):342-374
Zheng YF and Hermann J.2014.Geochemistry of continental subductionzone fluids.Earth,Planets and Space,66(1):93
梁金龙,孙晓明,徐莉,翟伟,汤倩,梁业恒.2006.CCSD及青龙山HP-UHP变质岩中绿帘石地球化学及其对板块折返过程的示踪.岩石学报,22(7):1845-1854
魏春景,崔莹.2011.地壳俯冲与折返过程的变质作用演化:来自高压-超高压榴辉岩相平衡模拟的证据.岩石学报,27(4):1067-1074
肖益林,余成龙,王洋洋,陆一敢.2018.变质作用与流体包裹体:进展与展望.矿物岩石地球化学通报,37(3):424-440
翟伟,孙晓明,梁金龙,徐莉,汤倩,梁业恒,苏丽薇.2006.青龙山超高压变质榴辉岩绿帘石化学成分与流体包裹体特征.岩石学报,22(7):2029-2038
张泽明,张金凤,游振东,沈昆.2005.苏鲁造山带超高压变质作用及其P-T-t轨迹.岩石学报,21(2):257-270
张泽明,沈昆.2009.大陆俯冲带的深部流体及变质化学地球动力学---以苏鲁超高压变质带为例.地球学报,30(1):5-20
Andersen T,Austrheim H,Burke EAJ and Elvevold S.1993.N2and CO2in deep crustal fluids:Evidence from the Caledonides of Norway.Chemical Geology,108(1-4):113-132
Angiboust S,Pettke T,De Hoog JCM,Caron B and Oncken O.2014.Channelized fluid flow and eclogite-facies metasomatism along the subduction shear zone.Journal of Petrology,55(5):883-916
Arculus RJ.1985.Oxidation status of the mantle:Past and present.Annual Review of Earth and Planetary Sciences,13:75-95
Armbruster T,Bonazzi P,Akasaka M,Bermanec V,Chopin C,GieréR,Heuss-Assbichler S,Liebscher A,Menchetti S,Pan YM and Pasero M.2006.Recommended nomenclature of epidote-group minerals.European Journal of Mineralogy,18(5):551-567
Austrheim H.1987.Eclogitization of lower crustal granulites by fluid migration through shear zones.Earth and Planetary Science Letters,81(2-3):221-232
Bebout GE.2007.Metamorphic chemical geodynamics of subduction zones.Earth and Planetary Science Letters,260(3-4):373-393
Becker H,Jochum KP and Carlson RW.1999.Constraints from highpressure veins in eclogites on the composition of hydrous fluids in subduction zones.Chemical Geology,160(4):291-308
Beinlich A,Klemd R,John T and Gao J.2010.Trace-element mobilization during Ca-metasomatism along a major fluid conduit:Eclogitization of blueschist as a consequence of fluid-rock interaction.Geochimica et Cosmochimica Acta,74(6):1892-1922
Bermanec V,Armbruster T,Oberhnsli R and Zebec V.1994.Crystal chemistry of Pb-and REE-rich piemontite from Nezilovo,Macedonia.Schweizerische Mineralogische und Petrographische Mitteilungen,74:321-328
Bieseler B,Diehl A,J9ns N,Lucassen F and Bach W.2018.Constraints on cooling of the lower ocean crust from Epidote veins in the Wadi Gideah Section,Oman ophiolite.Geochemistry,Geophysics,Geosystems,19(11):4195-4217
Bonazzi P and Menchetti S.2004.Manganese in monoclinic members of the epidote group:Piemontite and related minerals.Reviews in Mineralogy and Geochemistry,56(1):495-552
Brastad K.1985.Sr metasomatism,and partition of Sr between the mineral phases of a meta-eclogite from Bjrkedalen,West Norway.Tschermaks Mineralogische und Petrographische Mitteilungen,34(2):87-103
Brenan JM,Ryerson FJ and Shaw HF.1998.The role of aqueous fluids in the slab-to-mantle transfer of boron,beryllium,and lithium during subduction:Experiments and models.Geochimica et Cosmochimica Acta,62(19-20):3337-3347
Brovarone AV and Beyssac O.2014.Lawsonite metasomatism:A new route for water to the deep earth.Earth and Planetary Science Letters,393:275-284
Brovarone AV,Chu X,Martin L,Ague JJ,MoniéP,Groppo C,Martinez I and Chaduteau C.2018.Intra-slab COH fluid fluxes evidenced by fluid-mediated decarbonation of lawsonite eclogitefacies altered oceanic metabasalts.Lithos,304-307:211-229
Brunsmann A,Franz G,Erzinger J and Landwehr D.2000.Zoisite-and clinozoisite-segregations in metabasites(Tauern Window,Austria)as evidence for high-pressure fluid-rock interaction.Journal of Metamorphic Geology,18(1):1-21
Brunsmann A,Franz G and Erzinger J.2001.REE mobilization during small-scale high-pressure fluid-rock interaction and zoisite/fluid partitioning of La to Eu.Geochimica et Cosmochimica Acta,65(4):559-570
Brunsmann A,Franz G and Heinrich W.2002.Experimental investigation of zoisite-clinozoisite phase equilibria in the system CaO-Fe2O3-Al2O3-SiO 2-H2O.Contributions to Mineralogy and Petrology,143(1):115-130
Campos-Alvarez NO,Samson IM,Fryer BJ and Ames DE.2010.Fluid sources and hydrothermal architecture of the Sudbury Structure:Constraints from femtosecond LA-MC-ICP-MS Sr isotopic analysis of hydrothermal epidote and calcite.Chemical Geology,278(3-4):131-150
Cao MJ,Qin KZ,Li GM,Evans NJ,McI nnes BIA,Li JX and Zhao JX.2018.Oxidation state inherited from the magma source and implications for mineralization:Late Jurassic to Early Cretaceous granitoids,Central Lhasa subterrane,Tibet.Mineralium Deposita,53(3):299-309
Cao Y,Song SG,Niu YL,Jung H and Jin ZM.2011.Variation of mineral composition,fabric and oxygen fugacity from massive to foliated eclogites during exhumation of subducted ocean crust in the North Qilian suture zone,NW China.Journal of Metamorphic Geology,29(7):699-720
Castelli D,Rolfo F,Compagnoni R and Xu ST.1998.Metamorphic veins with kyanite,zoisite and quartz in the Zhujiachong eclogite,Dabie Shan,China.Island Arc,7(1-2):159-173
Chen RX,Zheng YF and Hu ZC.2012.Episodic fluid action during exhumation of deeply subducted continental crust:Geochemical constraints from zoisite-quartz vein and host metabasite in the Dabie orogen.Lithos,155:146-166
Chen YX,Zheng YF,Gao XY and Hu ZC.2014.Multiphase solid inclusions in zoisite-bearing eclogite:Evidence for partial melting of ultrahigh-pressure metamorphic rocks during continental collision.Lithos,200-201:1-21
Choo CO.2002.Complex compositional zoning in epidote from rhyodacitic tuff,Bobae sericite deposit,Southeastern Korea.Journal of Mineralogy and Geochemistry,177(2):181-197
Clarke GL,Powell R and Fitzherbert JA.2006.The lawsonite paradox:A comparison of field evidence and mineral equilibria modelling.Journal of Metamorphic Geology,24(8):715-725
Davies JH.1999.The role of hydraulic fractures and intermediate-depth earthquakes in generating subduction-zone magmatism.Nature,398(6723):142-145
Davis PB and Whitney DL.2006.Petrogenesis of lawsonite and epidote eclogite and blueschist,Sivrihisar Massif,Turkey.Journal of Metamorphic Geology,24(9):823-849
Deer WA,Howie RA and Zussman J.1986.Rock-Forming Minerals,Vol 1B,Disilicates and Ring Silicates.2ndEdition.New York:Longman,1-629
Donohue CL and Essene EJ.2000.An oxygen barometer with the assemblage garnet-epidote.Earth and Planetary Science Letters,181(3):459-472
Eide EA and Liou JG.2000.High-pressure blueschists and eclogites in Hong’an:A framework for addressing the evolution of high-and ultrahigh-pressure rocks in central China.Lithos,52(1-4):1-22
El Korh A,Schmidt ST,Ulianov A and Potel S.2009.Trace element partitioning in HP-LT metamorphic assemblages during subductionrelated metamorphism,Ile de Groix,France:A detailed LA-ICPMSstudy.Journal of Petrology,50(6):1107-1148
Enami M,Liou JG and Mattinson CG.2004.Epidote minerals in high P/T metamorphic terranes:Subduction zone and high-to ultrahighpressure metamorphism.Reviews in Mineralogy and Geochemistry,56(1):347-398
Eskola PE.1933.On the chrome minerals of Outokumpu.Bulletin de la Comission Gèologique de Finlande,103:26-44
Feineman MD,Ryerson FJ,DeP aolo DJ and Plank T.2007.Zoisiteaqueous fluid trace element partitioning with implications for subduction zone fluid composition.Chemical Geology,239(3-4):250-265
Finger F,Broska I,Roberts MP and Schermaier A.1998.Replacement of primary monazite by apatite-allanite-epidote coronas in an amphibolite facies granite gneiss from the eastern Alps.AmericanMineralogist,83(3-4):248-258
Frank MR,Candela PA,Piccoli PM and Glascock MD.2002.Gold solubility,speciation,and partitioning as a function of HCL in the brine-silicate melt-metallic gold system at 800℃and 100MPa.Geochimica et Cosmochimica Acta,66(21):3719-3732
Franz G and Liebscher A.2004.Physical and chemical properties of the epidote minerals:An introduction.Reviews in Mineralogy and Geochemistry,56(1):1-81
Franz L,Romer RL,Klemd R,Schimd R,Oberhnsli R,Wagner T and Dong SW.2001.Eclogite-facies quartz veins within metabasites of the Dabie Shan(eastern China):Pressure-temperature-timedeformation path,composition of the fluid phase and fluid flow during exhumation of high-pressure rocks.Contributions to Mineralogy and Petrology,141(3):322-346
Frei D,Liebscher A,Franz G and Dulski P.2004.Trace element geochemistry of epidote minerals.Reviews in Mineralogy and Geochemistry,56(1):553-605
Fu B,Touret JLR and Zheng YF.2001.Fluid inclusions in coesitebearing eclogites and jadeite quartzite at Shuanghe,Dabie Shan(China).Journal Metamorphic Geology,19(5):531-547
Gao J and Klemd R.2001.Primary fluids entrapped at blueschist to eclogite transition:Evidence from the Tianshan meta-subduction complex in northwestern China.Contributions to Mineralogy and Petrology,142(1):1-14
Gao J,John T,Klemd R and Xiong XM.2007.Mobilization of Ti-Nb-Ta during subduction:Evidence from rutile-bearing dehydration segregations and veins hosted in eclogite,Tianshan,NW China.Geochimica et Cosmochimica Acta,71(20):4974-4996
Gao XY,Zheng YF and Chen YX.2012.Dehydration melting of ultrahigh-pressure eclogite in the Dabie orogen:Evidence from multiphase solid inclusions in garnet.Journal of Metamorphic Geology,30(2):193-212
Gatta GD,Merlini M,Lee Y and Poli S.2011.Behavior of epidote at high pressure and high temperature:A powder diffraction study up to10GPa and 1,200K.Physics and Chemistry of Minerals,38(6):419-428
GieréR and Sorensen SS.2004.Allanite and other REE-rich epidotegroup minerals.Reviews in Mineralogy and Geochemistry,56(1):431-493
Gottschalk M.2004.Thermodynamic properties of zoisite,clinozoisite and epidote.Reviews in Mineralogy and Geochemistry,56(1):83-124
Grapes RH.1981.Chromian epidote and zoisite in kyanite amphibolite,Southern Alps,New Zealand.American Mineralogist,66:974-975
Grapes RH and Watanabe T.1984.Al-Fe3+and Ca-Sr2+epidotes in metagreywacke-quartzofeldspathic schist,Southern Alps,New Zealand.American Mineralogist,69:490-498
Grapes RH and Hoskin PWO.2004.Epidote group minerals in lowmedium pressure metamorphic terranes.Reviews in Mineralogy and Geochemistry,56(1):301-345
Guo HH,Xiao YL,Xu LJ,Sun H,Huang J and Hou ZH.2017a.Origin of allanite in gneiss and granite in the Dabie orogenic belt,Central East China.Journal of Asian Earth Sciences,135:243-256
Guo S,Ye K,Chen Y,Liu JB,Mao Q and Ma YG.2012.Fluid-rock interaction and element mobilization in UHP metabasalt:Constraints from an omphacite-epidote vein and host eclogites in the Dabie orogen.Lithos,136-139:145-167
Guo S,Ye K,Wu TF,Chen Y,Yang YH,Zhang LM,Liu JB,Mao Qand Ma YG.2013.A potential method to confirm the previous existence of lawsonite in eclogite:The mass imbalance of Sr and LREEs in multistage epidote(Ganghe,Dabie UHP terrane).Journal of Metamorphic Geology,31(4):415-435
Guo S,Ye K,Yang YH,Chen Y,Zhang LM,Liu JB,Mao Q and Ma YG.2014.In situ Sr isotopic analyses of epidote:Tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite(Ganghe,Dabie terrane).Contributions to Mineralogy and Petrology,167(2):975
Guo S,Chen Y,Ye K,Su B,Yang YH,Zhang LM,Liu JB and Mao Q.2015a.Formation of multiple high-pressure veins in ultrahighpressure eclogite(Hualiangting,Dabie terrane,China):Fluid source,element transfer,and closed-system metamorphic veining.Chemical Geology,417:238-260
Guo S,Ye K,Cheng NF,Chen Y,Su B and Liu JB.2015b.Metamorphic P-T trajectory and multi-stage fluid events of veinbearing UHP eclogites from the Dabie terrane:Insights from compositional zonations of key minerals.International Geology Review,57(9-10):1077-1102
Guo S,Yang YH,Chen Y,Su B,Gao YJ,Zhang LM,Liu JB and Mao Q.2016.Grainscale Sr isotope heterogeneity in amphibolite(retrograded UHP eclogite,Dabie terrane):Implications for the origin and flow behavior of retrograde fluids during slab exhumation.Lithos,266-267:383-405
Guo S,Tang P,Su B,Chen Y,Ye K,Zhang LM,Gao YJ,Liu JB and Yang YH.2017b.Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins(Dabie UHPterrane):A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs.American Mineralogist,102(11):2268-2283
Guo S,Zhao KD,John T,Tang P,Chen Y and Su B.2019.Metasomatic flow of metacarbonate-derived fluids carrying isotopically heavy boron in continental subduction zones:Insights from tourmaline-bearing ultra-high pressure eclogites and veins(Dabie terrane,eastern China).Geochimica et Cosmochimica Acta,253:159-200
Hacker BR,Peacock SM,Abers GA and Holloway SD.2003.Subduction factory 2.Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions?Journal of Geophysical Research,108(B1):2030
Harris C,Hlongwane W,Gule N and Scheepers R.2014.Origin of tanzanite and associated gemstone mineralization at Merelani,Tanzania.South African Journal of Geology,117(1):15-30
Haüy RJ.1801.Traitéde Minérologie.Chez Louis Libraire,Paris,102-113
Hermann J.2002.Allanite:Thorium and light rare earth element carrier in subducted crust.Chemical Geology,192(3-4):289-306
Hermann J,Spandler C,Hack A and Korsakov AV.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
Hirajima T,Zhang R,Li J and Cong B.1992.Petrology of the nyb9itebearing eclogite in the Donghai area,Jiangsu Province,eastern China.Mineralogical Magazine,56(382):37-46
Holdaway MJ.1972.Thermal stability of AI-Fe epidote as a function of fOand Fe content.Contributions to Mineralogy and Petrology2,37(4):307-340
Hu HY,Dai LD,Li HP,Hui KS and Sun WQ.2017.Influence of dehydration on the electrical conductivity of epidote and implications for high-conductivity anomalies in subduction zones.Journal of Geophysical Research:Solid Earth,122:2751-2762
Huang J,Xiao Y,Gao Y,Hou Z and Wu W.2012.Nb-Ta fractionation induced by fluid-rock interaction in subduction-zones:Constraints from UHP eclogite-and vein-hosted rutile from the Dabie orogen,Central-Eastern China.Journal of Metamorphic Geology,30(8):821-842
Jan cˇev S and Bermanec V.1998.Solid solution between epidote and hancockite from Nezilovo,Macedonia.Geologia Croatica,51(1):23-26
John T,Scherer EE,Haase KM and Schenk V.2004.Trace element fractionation during fluid-induced eclogitization in a subducting slab:Trace element and Lu-Hf-Sm-Nd isotope systematics.Earth and Planetary Science Letters,227(3-4):441-456
John T,Klemd R,Gao J and Garbe-Sch9nberg CD.2008.Trace-element mobilization in slabs due to non steady-state fluid-rock interaction:Constraints from an eclogite-facies transport vein in blueschist(Tianshan,China).Lithos,103(1-2):1-24
John T,Gussone N,Podladchikov YY,Bebout GE,Dohmen R,Halama R,Klemd R,Magna T and Seitz HM.2012.Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs.Nature Geoscience,5(7):489-492
Klemd R.2004.Fluid inclusions in epidote minerals and fluid development in epidote-bearing rocks.Reviews in Mineralogy and Geochemistry,56(1):197-234
Klemd R.2012.Metasomatism during high-pressure metamorphism:Eclogites and blueschist-facies rocks.In:Harlov DE and Austrheim H(eds.).Metasomatism and the Chemical Transformation of Rock:The Role of Fluids in Terrestrial and Extraterrestrial Processes.Berlin Heidelberg:Springer-Verlag,351-413
Korsakov AV and Hermann J.2006.Silicate and carbonate melt inclusions associated with diamonds in deeply subducted carbonate rocks.Earth and Planetary Science Letters,241(1-2):104-118
Li JL,Gao J,John T,Klemd R and Su W.2013.Fluid-mediated metal transport in subduction zones and its link to arc-related giant ore deposits:Constraints from a sulfide-bearing HP vein in lawsonite eclogite(Tianshan,China).Geochimica et Cosmochimica Acta,120:326-362
Li XP,Zheng YF,Wu YB,Chen FK,Gong B and Li YL.2004.Low-Teclogite in the Dabie terrane of China:Petrological and isotopic constraints on fluid activity and radiometric dating.Contributions to Mineralogy and Petrology,148(4):443-470
Li YL,Zheng YF,Fu B,Zhou JB and Wei CS.2001.Oxygen isotope composition of quartz-vein in ultrahigh-pressure eclogite from Dabieshan and implications for transport of high-pressure metamorphic fluid.Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,26(9-10):695-704
Liang JL,Sun XM,Xu L,Zhai W,Tang Q and Liang YH.2006.Geochemistry of epidotes in HP-UHP metamorphic rocks from Chinese Continental Scientific Drilling(CCSD)Project and Qinglongshan area:An indicator of partial melting during continental slab exhumation.Acta Petrologica Sinica,22(7):1845-1854(in Chinese with English abstract)
Liou JG.1973.Synthesis and stability relations of epidote,Ca2Al2FeS i3O12(OH).Journal of Petrology,14(3):381-413
Liou JG,Kim HS and Maruyama S.1983.Prehnite-epidote equilibria and their petrologic applications.Journal of Petrology,24(4):321-342
Liu FL,Gerdes A,Liou JG,Xue HM and Liang FH.2006.SHRIMP U-Pb zircon dating from Sulu-Dabie dolomitic marble,eastern China:Constraints on prograde,ultrahigh-pressure and retrograde metamorphic ages.Journal of Metamorphic Geology,24(7):569-589
Liu PL,Wu Y,Chen Y,Zhang JF and Jin ZM.2015.UHP impure marbles from the Dabie Mountains:Metamorphic evolution and carbon cycling in continental subduction zones.Lithos,212-215:280-297
Liu PL,Zhang JF,Massonne HJ and Jin ZM.2018.Polyphase solidinclusions formed by interactions between infiltrating fluids and precursor minerals enclosed in garnet of UHP rocks from the Dabie Shan,China.American Mineralogist,103(10):1663-1673
Liu XC,Dong SW,Xue HM and Zhou JX.1999.Significance of allanite-(Ce)in granitic gneisses from the ultrahigh-pressure metamorphic terrane,Dabie Shan,central China.Mineralogical Magazine,63(4):579-586
Liu XC,Jahn BM,Dong SW,Li HM and Oberhnsli R.2003.Neoproterozoic granitoid did not record ultrahigh-pressure metamorphism from the southern Dabieshan of China.The Journal of Geology,111(6):719-732
Malisa EPJ.2003.Trace elements characterization of the hydrothermally deposited tanzanite and green grossular in the Merelani-Lelatema shear zone,northeastern Tanzania.Tanzania Journal of Science,29(1):45-60
Manning CE.2004.The chemistry of subduction-zone fluids.Earth and Planetary Science Letters,223(1-2):1-16
Martin LAJ,Wood BJ,Turner S and Rushmer T.2011.Experimentalmeasurements of trace element partitioning between lawsonite,zoisite and fluid and their implication for the composition of arc magmas.Journal of Petrology,52(6):1049-1075
Massonne HJ and O’Brien PJ.2003.The Bohemian massif and the NWHimalaya.In:Carswell DA,Compagnoni R and Rolfo F(eds.).Ultrahigh Pressure Metamorphism.European Mineralogical Union Notes in Mineralogy,5:145-188
Massonne HJ.2012.Formation of amphibole and clinozoisite-epidote in eclogite owing to fluid infiltration during exhumation in a subduction channel.Journal of Petrology,53(10):1969-1998
Mattinson CG,Zhang RY,Tsujimori T and Liou JG.2004.Epidote-rich talc-kyanite-phengite eclogites,Sulu terrane,eastern China:P-T-fOestimates and the significance of the epidote-talc assemblage in2eclogite.American Mineralogist,89(11-12):1772-1783
McC ulloch MT and Gamble JA.1991.Geochemical and geodynamical constraints on subduction zone magmatism.Earth and Planetary Science Letters,102(3-4):358-374
Mengason MJ,Candela PA and Piccoli PM.2011.Molybdenum,tungsten and manganese partitioning in the system pyrrhotite-Fe-S-Omelt-rhyolite melt:Impact of sulfide segregation on arc magma evolution.Geochimica et Cosmochimica Acta,75(22):7018-7030
Miyajima H,Matsubara S,Miyawaki R and Hirokawa K.2003.Niigataite,CaSrAl3(Si2O7)(SiO 4)O(OH):Sr-analogue of clinozoisite,a new member of the epidote group from the ItoigawaOhmi district,Niigata Prefecture,central Japan.Journal of Mineralogical and Petrological Sciences,98(3):118-129
Miyashiro A and Seki Y.1958.Enlargement of the composition field of epidote and piemontite with rising temperature.American Journal of Science,256(6):423-430
Mungall JE.2002.Roasting the mantle:Slab melting and the genesis of major Au and Au-rich Cu deposits.Geology,30(10):915-918
Nagasaki A and Enami M.1998.Sr-bearing zoisite and epidote in ultrahigh pressure(UHP)metamorphic rocks from the Su-Lu provinces,eastern China:An important Sr reservoir under UHP conditions.American Mineralogist,83(3-4):240-247
Nagashima M,Akasaka M and Sakurai T.2006.Chromian epidote in omphacite rocks from the Sambagawa metamorphic belt,central Shikoku,Japan.Journal of Mineralogical and Petrological Sciences,101(4):157-169
Nagashima M,Nishio-Hamane D,Nakano N and Kawasaki T.2019.Synthesis and crystal chemistry of mukhinite,V-analogue of clinozoisite on the join Ca2Al3Si3O12(OH)-Ca2Al2VSi3O12(OH).Physics and Chemistry of Minerals,46(1):63-76
Naney MT.1983.Phase equilibria of rock-forming ferromagnesian silicates in granitic systems.American Journal of Science,283(10):993-1033
Ni HW,Zheng YF,Mao Z,Wang Q,Chen RX and Zhang L.2017.Distribution,cycling and impact of water in the Earth’s interior.National Science Review,4(6):879-891
Oh CW,Liou JG and Maruyama S.1991.Low-temperature eclogites and eclogitic schists in Mn-rich metabasites in Ward Creek,California:Mn and Fe effects on the transition between blueschist and eclogite.Journal of Petrology,32(2):275-302
Pawley AR.1994.The pressure and temperature stability limits of lawsonite:Implications for H2O recycling in subduction zones.Contributions to Mineralogy and Petrology,118(1):99-108
Peacock SA.1990.Fluid processes in subduction zones.Science,248(4953):329-337
Poli S and Schmidt MW.1995.H2O transport and release in subduction zones:Experimental constraints on basaltic and andesitic systems.Journal of Geophysical Research:Solid Earth,100(B11):22299-22314
Poli S and Schmidt MW.1998.The high-pressure stability of zoisite and phase relationships of zoisite-bearing assemblages.Contributions to Mineralogy and Petrology,130(2):162-175
Poli S and Schmidt MW.2004.Experimental subsolidus studies on epidote minerals.Epidotes.Reviews in Mineralogy andGeochemistry,56(1):171-195
Poli S.2016.Melting carbonated epidote eclogites:Carbonatites from subducting slabs.Progress in Earth and Planetary Science,3:27
Potel S,Schmidt ST and de Capitani C.2002.Composition of pumpellyite,epidote and chlorite from New Caledonia:How important are metamorphic grade and whole-rock composition?Schweizerische Mineralogische und Petrographische Mitteilungen,82(1):229-252
Rolfo F,Compagnoni R,Xu ST and Jiang LL.2000.First report of felsic whiteschist in the ultrahigh-pressure metamorphic belt of Dabie Shan,China.European Journal of Mineralogy,12(4):883-898
Romer RL and Xiao YL.2005.Initial Pb-Sr(-Nd)isotopic heterogeneity in a single allanite-epidote crystal:Implications of reaction history for the dating of minerals with low parent-to-daughter ratios.Contributions to Mineralogy and Petrology,148(6):662-674
Rubatto D,Williams IS and Buick IS.2001.Zircon and monazite response to prograde metamorphism in the Reynolds Range,central Australia.Contributions to Mineralogy and Petrology,140(4):458-468
Rubatto D and Hermann J.2003.Zircon formation during fluid circulation in eclogites(Monviso,Western Alps):Implications for Zr and Hf budget in subduction zones.Geochimica et Cosmochimica Acta,67(12):2173-2187
Rubatto D and Angiboust S.2015.Oxygen isotope record of oceanic and high-pressure metasomatism:A P-T-time-fluid path for the Monviso eclogites(Italy).Contributions to Mineralogy and Petrology,170(5-6):44
Santosh M,Tsunogae T,Shimizu H and Dubessy J.2010.Fluid characteristics of retrogressed eclogites and mafic granulites from the Cambrian Gondwana suture zone in southern India.Contributions to Mineralogy and Petrology,159(3):349-369
Sassi R,Harte B,Carswell DA and Yujing H.2000.Trace element distribution in Central Dabie eclogites.Contributions to Mineralogy and Petrology,139(3):298-315
Scambelluri M and Philippot P.2001.Deep fluids in subduction zones.Lithos,55(1-4):213-227
Schmidt MW and Poli S.1994.The stability of lawsonite and zoisite at high pressures:Experiments in CASH to 92kbar and implications for the presence of hydrous phases in subducted lithosphere.Earth and Planetary Science Letters,124(1-4):105-118
Schmidt MW and Thompson AB.1996.Epidote in calc-alkaline magmas:An experimental study of stability,phase relationships,and the role of epidote in magmatic evolution.American Mineralogist,81(3-4):462-474
Schmidt MW and Poli S.1998.Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation.Earth and Planetary Science Letters,163(1-4):361-379
Sheng YM,Zheng YF,Chen RX,Li QL and Dai MN.2012.Fluid action on zircon growth and recrystallization during quartz veining within UHP eclogite:Insights from U-Pb ages,O-Hf isotopes and trace elements.Lithos,136-139:126-144
Skjerlie KP and Pati1o Douce AE.2002.The fluid-absent partial melting of a zoisite-bearing quartz eclogite from 1.0 to 3.2GPa:Implications for melting in thickened continental crust and for subduction-zone processes.Journal of Petrology,43(2):291-314
Sobolev NV and Shatsky VS.1990.Diamond inclusions in garnets from metamorphic rocks:A new environment for diamond formation.Nature,343(6260):742-746
Song SG,Niu YL,Su L,Wei CJ and Zhang LF.2014.Adakitic(tonalitic-trondhjemitic)magmas resulting from eclogite decompression and dehydration melting during exhumation in response to continental collision.Geochimica et Cosmochimica Acta,130:42-62
Sorensen SS and Grossman JN.1989.Enrichment of trace elements in garnet amphibolites from a paleo-subduction zone:Catalina Schist,southern California.Geochimica et Cosmochimica Acta,53(12):3155-3177
Spandler C,Hermann J,Arculus R and Mavrogenes J.2003.Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies:Implications for deep subduction-zone processes.Contributions to Mineralogy and Petrology,146(2):205-222
Spandler C,Pettke T and 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.Journal of Petrology,52(6):1207-1236
Spiegel C,Siebel W,Frisch W and Berner Z.2002.Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators:Implications for the reconstruction of the exhumation history of the Central Alps.Chemical Geology,189(3-4):231-250
Sun WD,Arculus RJ,Kamenetsky VS and Binns RA.2004.Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization.Nature,431(7011):975-978
Svensen H,Jamtveit B,Banks DA and Austrheim H.2001.Halogen contents of eclogite facies fluid inclusions and minerals:Caledonides,western Norway.Journal of Metamorphic Geology,19(2):165-178
Tatsumi Y and Eggins S.1995.Subduction Zone Magmatism.Cambridge,MA:Blackwell Science
Teyssier C,Whitney DL,Toraman E and Seaton NCA.2010.Lawsonite vorticity and subduction kinematics.Geology,38(12):1123-1126
Treloar PJ.1987a.Chromian muscovites and epidotes from Outokumpu,Finland.Mineralogical Magazine,51(62):593-599
Treloar PJ.1987b.The Cr-minerals of Outokumpu:Their chemistry and significance.Journal of Petrology,28(5):867-886
Tumiati S,Godard G,Martin S,Nimis P,Mair V and Boyer B.2005.Dissakisite-(La)from the Ulten zone peridotite(Italian Eastern Alps):A new end-member of the epidote group.American Mineralogist,90(7):1177-1185
Uher P,Kovácˇik M,Kubi2 M,Shtukenberg A and Ozd'n D.2008.Metamorphic vanadian-chromian silicate mineralization in carbon-rich amphibole schists from the MaléKarpaty Mountains,Western Carpathians,Slovakia.American Mineralogist,93(1):63-73
van der Straaten F,Schenk V,John T and Gao J.2008.Blueschistfacies rehydration of eclogites(Tian Shan,NW-China):Implications for fluid-rock interaction in the subduction channel.Chemical Geology,255(1-2):195-219
Verlaguet A,GofféB,Brunet F,Poinssot C,Vidal O,Findling N and Menut D.2011.Metamorphic veining and mass transfer in a chemically closed system:A case study in Alpine metabauxites(western Vanoise).Journal of Metamorphic Geology,29(3):275-300
Volkova NI,Frenkel AE,Budanov VI and Lepezin GG.2004.Geochemical signatures for eclogite protolith from the Maksyutov Complex,South Urals.Journal of Asian Earth Sciences,23(5):745-759
Vrijmoed JC,Austrheim H,John T,Hin RC,Corfu F and Davies GR.2013.Metasomatism in the ultrahigh-pressure Svartberget garnetsperidotite(Western Gneiss Region,Norway):Implications for the transport of crust-derived fluids within the mantle.Journal of Petrology,54(9):1815-1848
Wang SJ,Wang L,Brown M,Piccoli PM,Johnson TE,Feng P,Deng H,Kitajima K and Huang Y.2017.Fluid generation and evolution during exhumation of deeply subducted UHP continental crust:Petrogenesis of composite granite-quartz veins in the Sulu belt,China.Journal of Metamorphic Geology,35(6):601-629
Watenphul A,Schmidt C and Jahn S.2014.Cr(Ⅲ)solubility in aqueous fluids at high pressures and temperatures.Geochimica et Cosmochimica Acta,126:212-227
Wei CJ,Li YJ,Yu Y and Zhang JS.2010.Phase equilibria and metamorphic evolution of glaucophane-bearing UHP eclogites from the Western Dabieshan Terrane,Central China.Journal of Metamorphic Geology,28(6):647-666
Wei CJ and Clarke GL.2011.Calculated phase equilibria for MORBcompositions:A reappraisal of the metamorphic evolution oflawsonite eclogite.Journal of Metamorphic Geology,29(9):939-952
Wei CJ and Cui Y.2011.Metamorphic evolution during subduction and exhumation of crust:Evidence from phase equilibria modelling for high-and ultrahigh-pressure eclogites.Acta Petrologica Sinica,27(4):1067-1074(in Chinese with English abstract)
Whitney DL and Davis PB.2006.Why is lawsonite eclogite so rare?Metamorphism and preservation of lawsonite eclogite,Sivrihisar,Turkey.Geology,34(6):473-476
Whitney DL and Evans BW.2010.Abbreviations for names of rockforming minerals.American Mineralogist,95(1):185-187
Wu YB,Gao S,Zhang HF,Yang SH,Liu XC,Jiao WF,Liu YS,Yuan HL,Gong HJ and He MC.2009.U-Pb age,trace-element,and Hfisotope compositions of zircon in a quartz vein from eclogite in the western Dabie Mountains:Constraints on fluid flow during early exhumation of ultrahigh-pressure rocks.American Mineralogist,94(2-3):303-312
Xia QK,Liu J,Kovács I,Hao YT,Li P,Yang XZ,Chen H and Sheng YM.2019.Water in the upper mantle and deep crust of eastern China:Concentration,distribution and implications.National Science Review,6(1):125-144
Xiao YL,Hoefs J,van den Kerkhof AM,Fiebig J and Zheng YF.2000.Fluid history of UHP metamorphism in Dabie Shan,China:A fluid inclusion and oxygen isotope study on the coesite-bearing eclogite from Bixiling.Contributions to Mineralogy and Petrology,139(1):1-16
Xiao YL,Hoefs J,Hou ZH,Simon K and Zhang ZM.2011.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.Contributions to Mineralogy and Petrology,162(4):797-819
Xiao YL,Sun H,Gu HO,Huang J,Li WY and Liu L.2015.Fluid/melt in continental deep subduction zones:Compositions and related geochemical fractionations.Science China(Earth Sciences),58(9):1457-1476
Xiao YL,Yu CL,Wand YY and Lu YG.2018.Metamorphism and fluid inclusions:An overview and prospectives.Bulletin of Mineralogy,Petrology and Geochemistry,37(3):424-440(in Chinese with English abstract)
Yang JJ and Enami M.2003.Chromian dissakisite-(Ce)in a garnet lherzolite from the Chinese Su-Lu UHP metamorphic terrane:Implications for Cr incorporation in epidote-group minerals and recycling of REE into the Earth’s mantle.American Mineralogist,88(4):604-610
Yao YP,Ye K,Liu JB,Cong BL and Wang QC.2000.A transitional eclogite-to high pressure granulite-facies overprint on coesite-eclogite at Taohang in the Sulu ultrahigh-pressure terrane,eastern China.Lithos,52(1-4):109-120
Zack T,Rivers T,Brumm R and Kronz A.2004.Cold subduction of oceanic crust:Implications from a lawsonite eclogite from the Dominican Republic.European Journal of Mineralogy,16(6):909-916
Zhai W,Sun XM,Liang JL,Xu L,Tang Q,Liang YH and Su LW.2006.Chemical compositions and fluid inclusions of epidotes in Qinglongshan ultrahigh pressure metamorphic eclogite,North Jiangsu Province,China.Acta Petrologica Sinica,22(7):2029-2038(in Chinese with English abstract)
Zhang HF,Gao S,Zhong ZQ,Zhang BR,Zhang L and Hu SH.2002.Geochemical and Sr-Nd-Pb isotopic compositions of Cretaceous granitoids:Constraints on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt,China.Chemical Geology,186(3-4):281-299
Zhang RY.1992.Petrogenesis of high pressure metamorphic rocks in the Su-Lu and Dianxi regions,China.Ph.D.Dissertation.Kyoto:Kyoto University,1-176
Zhang RY,Hirajima T,Banno S,Cong B and Liou JG.1995.Petrology of ultrahigh-pressure rocks from the southern Su-Lu region,EasternChina.Journal of Metamorphic Geology,13(6):659-675
Zhang RY,Liou JG,Ernst WG,Coleman RG,Sobolev NV and Shatsky VS.1997.Metamorphic evolution of diamond-bearing and associated rocks from the Kokchetav Massif,northern Kazakhstan.Journal of Metamorphic Geology,15(4):479-496
Zhang ZM,Xiao YL,Liu FL,Liou JG and Hoefs J.2005.Petrogenesis of UHP metamorphic rocks from Qinglongshan,southern Sulu,eastcentral China.Lithos,81(1-4):189-207
Zhang ZM,Zhang JF,You ZD and Sheng K.2005.Ultrahigh-pressure metamorphic P-T-t path of the Sulu orogenic belt,eastern central China.Acta Petrologica Sinica,21(2):257-270(in Chinese with English abstract)
Zhang ZM,Shen K,Sun WD,Liu YS,Liou JG,Shi C and Wang JL.2008.Fluids in deeply subducted continental crust:Petrology,mineral chemistry and fluid inclusion of UHP metamorphic veins from the Sulu orogen,eastern China.Geochimica et Cosmochimica Acta,72(13):3200-3228
Zhang ZM and Shen K.2009.Fluids from the deeply continental subduction zone and the metamorphic chemical geodynamics.Acta Geoscientia Sinica,30(1):5-20(in Chinese with English abstract)
Zhao YJ,Wu YB,Liu XC,Gao S,Wang H,Zheng JP and Yang SH.2016.Distinct zircon U-Pb and O-Hf-Nd-Sr isotopic behaviour during fluid flow in UHP metamorphic rocks:Evidence from metamorphic veins and their host eclogite in the Sulu Orogen,China.Journal of Metamorphic Geology,34(4):343-362
Zheng YF,Gao TS,Wu YB,Gong B and Liu XM.2007.Fluid flow during exhumation of deeply subducted continental crust:Zircon U-Pb age and O-isotope studies of a quartz vein within ultrahighpressure eclogite.Journal of Metamorphic Geology,25(2):267-283
Zheng YF.2009.Fluid regime in continental subduction zones:Petrological insights from ultrahigh-pressure metamorphic rocks.Journal of the Geological Society,166(4):763-782
Zheng YF,Xia QX,Chen RX and Gao XY.2011.Partial melting,fluid supercriticality and element mobility in ultrahigh-pressure metamorphic rocks during continental collision.Earth-Science Reviews,107(3-4):342-374
Zheng YF and Hermann J.2014.Geochemistry of continental subductionzone fluids.Earth,Planets and Space,66(1):93
梁金龙,孙晓明,徐莉,翟伟,汤倩,梁业恒.2006.CCSD及青龙山HP-UHP变质岩中绿帘石地球化学及其对板块折返过程的示踪.岩石学报,22(7):1845-1854
魏春景,崔莹.2011.地壳俯冲与折返过程的变质作用演化:来自高压-超高压榴辉岩相平衡模拟的证据.岩石学报,27(4):1067-1074
肖益林,余成龙,王洋洋,陆一敢.2018.变质作用与流体包裹体:进展与展望.矿物岩石地球化学通报,37(3):424-440
翟伟,孙晓明,梁金龙,徐莉,汤倩,梁业恒,苏丽薇.2006.青龙山超高压变质榴辉岩绿帘石化学成分与流体包裹体特征.岩石学报,22(7):2029-2038
张泽明,张金凤,游振东,沈昆.2005.苏鲁造山带超高压变质作用及其P-T-t轨迹.岩石学报,21(2):257-270
张泽明,沈昆.2009.大陆俯冲带的深部流体及变质化学地球动力学---以苏鲁超高压变质带为例.地球学报,30(1):5-20