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个人简介

陈意,男,1980年12月出生于湖北黄冈市。研究员。 时间学校/工作单位名称专业学位/职称 1999.09-2003.07中国地质大学(武汉)地质学学士学位 2003.09-2008.07中科院地质与地球物理研究所矿物学、岩石学、矿床学博士学位 2008.07-2010.12中科院地质与地球物理研究所变质岩石学博士后 2011.02-2018.12中科院地质与地球物理研究所变质岩石学副研究员 2019.01-现今中科院地质与地球物理研究所变质岩石学研究员 承担科研项目情况: 中国科学院知识创新工程青年人才领域前沿项目,造山带石榴橄榄岩中钛斜粒硅镁石的成因及其对俯冲带高场强元素活动性的指示,2007.10-2009.09 国家自然科学基金青年基金(40902023):毛屋基性-超基性岩的变质演化及其对俯冲地壳流体与地幔楔相互作用的启示,2010.01-2012.12 国家自然科学基金面上项目(41372078):低温地幔楔底部对重稀土和高场强元素的过滤作用:对岛弧岩浆成因的启示,2014.01-2017.12 中国科学院战略性先导科技专项(B类)子课题(XDB03010202):新特提斯洋俯冲过程变质和超基性岩成因研究,2012.07-2017.06 国家重点基础研究发展计划(973)子课题(2015CB856103),超深俯冲陆壳对地幔楔的改造,2015/01-2019/12 国家自然科学基金重大项目课题(41490614),东西构造结大陆岩石圈俯冲的变质响应,2015/01-2019/12 国家自然科学基金优秀青年基金项目(41822202),变质岩石学,2019/01-2021/12 获奖及荣誉: 2008年获中国科学院“王宽诚博士后工作奖” 2018年获“侯德封矿物岩石地球化学青年科学家奖”

研究领域

主要从事板块俯冲及其改造的变质岩石学研究。 目前主要研究方向: 1.高压-超高压变质岩石学 2.俯冲带壳幔物质循环 3.高级变质岩热力学模拟

近期论文

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24.Su,B.,Chen,Y.*,Guo,S.,Chen,S.,Li,Y.B.,2019.Garnetiteandpyroxeniteinthemantlewedgeformedbyslab-mantleinteractionsatdifferentmelt/rockratios.JournalofGeophysicalResearch:SolidEarth,124,6504-6522.(通讯作者) 23.Su,B.,Chen,Y.*,Mao,Q.,Zhang,D.,Jia,L.H.,Guo,S.,2019.Minorelementsinolivineinspectthepetrogenesisoforogenicperidotites.Lithos,344–345,207–216.(通讯作者) 22.Su,B.,Chen,Y.*,Mao,Q.,2019.Sodiuminolivineasapotentialpressureindicatorfororogenicdunite.ScienceBulletin,doi:10.1016/j.scib.2019.10.007.(通讯作者) 21.陈意,2019。板块俯冲起始与成熟阶段的差异变质响应。矿物岩石地球化学通报,38(3):490–498. 20.张迪,陈意*,毛骞,苏斌,贾丽辉,郭顺,2019。电子探针分析技术进展及面临的挑战。岩石学报,35(1):261–274.(通讯作者) 19.Chen,Y.,Huang,F.,Shi,G.H.,Wu,F.Y.,Chen,X.,Jin,Q.Z.,Su,B.,Guo,S.,Sein,K.,Nyunt,T.T.,2018.MagnesiumisotopecompositionofsubductionzonefluidsasconstrainedbyjadeititesfromMyanmar.JournalofGeophysicalResearch:SolidEarth,123,7566–7585. 18.Su,B.,Chen,Y.*,2018.MakingCratonicLithosphericMantle.JournalofGeophysicalResearch:SolidEarth,123,7688–7706.(通讯作者) 17.陈意,陈思,苏斌,李仪兵,郭顺,2018。麻粒岩相金红石微量元素体系。地球科学,43(1),127–149. 16.Chen,Y.,Su,B.,Chu,Z.Y.,2017.Modificationofanancientsubcontinentallithosphericmantlebycontinentalsubduction:InsightfromtheMaowugarnetperidotitesintheDabieUHPbelt,easternChina.Lithos,278-281,54–71. 15.Su,B.,Chen,Y.*,Guo,S.,Liu,J.B.,2017.Dolomitedissociationindicatesultra-deep(>150km)subductionofagarnet-bearingduniteblock(theSuluUHPterrane).AmericanMineralogist,102,2295–2306(通讯作者). 14.王娟,陈意*,毛骞,李秋立,马玉光,石永红,宋传中,2017。金红石微量元素电子探针分析。岩石学报,33(6):1934–1946.(通讯作者) 13.Su,B.,Chen,Y.*,Guo,S.,Chu,Z.Y.,Liu,J.B.,Gao,Y.J.,2016.CarbonatiticmetasomatisminorogenicdunitesfromLijiatunintheSuluUHPterrane,easternChina.Lithos,262,266–284(通讯作者). 12.Su,B.,Chen,Y.*,Guo,S.,Liu,J.B.,2016.Originsoforogenicdunites:Petrology,geochemistry,andimplications.GondwanaResearch,29,41–59(通讯作者). 11.Chen,Y.,Su,B.,Guo,S.,2015.TheDabie-Suluorogenicperidotites:Progressandkeyissues.ScienceChinaEarthScience,58,1679–1699. 10.Chen,Y.,Ye,K.,Wu,T.F.,Guo,S.,2013.Exhumationofoceaniceclogites:thermodynamicconstraintsonpressure,temperature,bulkcompositionanddensity:JournalofMetamorphicGeology,31,549–570. 9.Chen,Y.,Ye,K.,Wu,Y.W.,Guo,S.,Su,B.,Liu,J.B.,2013.HydrationandDehydrationinthelowermarginofacoldmantlewedge:implicationsforcrust–mantleinteractionsandpetrogenesesofarcmagmas.InternationalGeologyReview,55,1506–1522. 8.Chen,Y.,Ye,K.,Guo,S.,Wu,T.F.,Liu,J.B.,2013,MultistagemetamorphismofgarnetorthopyroxenitesfromtheMaowumafic-ultramaficcomplex,DabieshanUHPterrane,easternChina.InternationalGeologyReview,55,1239–1260. 7.陈意,叶凯,苏斌,郭顺,刘景波。2013。大别-苏鲁造山带橄榄岩的变质和交代过程。科学通报,58(23):2294–2299. 6.陈意,叶凯。2013。俯冲洋壳的折返及其相关问题讨论。岩石学报,29(5):1451–1478。 5.Chen,Y.,Ye,K.,Liu,J.B.&Sun,M.,2008.QuantitativeP–T–Xconstraintsonorthopyroxene-bearinghigh-pressuregranulitesinfelsic-metapeliticrocks:evidencefromtheHuangtulinggranulite,DabieshanOrogen.JournalofMetamorphicGeology,26,1–15. 4.陈意,叶凯,刘景波,孙敏。2007。斜方辉石高压麻粒岩的成因研究进展。科学通报,52(22):2682。 3.Chen,Y.,Ye,K.,Liu,J.B.&Sun,M.,2006.MultistagemetamorphismoftheHuangtulinggranulite,NorthernDabieOrogen,easternChina:implicationsforthetectonometamorphicevolutionofsubductedlowercontinentalcrust.JournalofMetamorphicGeology,24,633–654. 2.陈意,叶凯,吴春明。2005。榴辉岩常用温压计在应用中应注意的问题。岩石学报,21:1067–1080。 1.陈意,金振民,欧新功,金淑燕,徐海军。2004。韧性剪切带中片麻岩和超高压榴辉岩变形特征及其与地震波速各向异性的关系:来自中国大陆科学钻探(CCSD)680–1200米岩心的证据。岩石学报,20:97–108。 合作作者论文 26.Guo,S.,Zhao,K.,John,T.,Tang,P.,Chen,Y.,Su,B.,2019.Metasomaticflowofmetacarbonate-derivedfluidscarryingisotopicallyheavyboronincontinentalsubductionzones:Insightsfromtourmaline-bearingultra-highpressureeclogitesandveins(Dabieterrane,easternChina).GeochimicaetCosmochimicaActa,253,159–200. 25.Guo,S.,Tang,P.,Su,B.,Chen,Y.,Ye,K.,Zhang,L.M.,Gao,Y.J.,Liu,J.B.,Yang,Y.H.,2017.UnusualreplacementofFe-Tioxidesbyrutileduringretrogressioninamphibolite-hostedveins(DabieUHPterrane):Amineralogicalrecordoffluid-inducedoxidationprocessesinexhumedUHPslabs.AmericanMineralogist,102,2268–2283. 24.Xu,Y.,Liu,C.Z.,Chen,Y.,Guo,S.,Wang,J.G.,Sein,K.,2017.PetrogenesisandtectonicimplicationsofgabbroandplagiograniteintrusionsinmantleperidotitesoftheMyitkyinaophiolite,Myanmar.Lithos,284,180–193. 23.Li,X.H.,Chen,Y.,Tchouankoue,J.P.,Liu,C.Z.,Li,J.,Ling,X.X.,Tang,G.Q.,Liu,Y.,2017.ImprovinggeochronologicalframeworkofthePan-AfricanorogenyinCameroon:NewSIMSzirconandmonaziteU-Pbageconstraints.PrecambrianResearch,294,307–321. 22.Guo,S.,Yang,Y.H.,Chen,Y.,Su,B.,Gao,Y.J.,Zhang,L.M.,Liu,J.B.,Mao,Q.,2016.Grain-scaleSrisotopeheterogeneityinamphibolite(retrogradedUHPeclogite,Dabieterrane):Implicationsfortheoriginandflowbehaviorofretrogradefluidsduringslabexhumation.Lithos,266,383–405. 21.Liu,C.Z.,Zhang,C.,Xu,Y.,Wang,J.G.,Chen,Y.,Guo,S.,Wu,F.Y.,Sein,K.,2016.PetrologyandgeochemistryofmantleperidotitesfromtheKalaymyoandMyitkyinaophiolites(Myanmar):Implicationsfortectonicsettings.Lithos,264,495–508. 20.Li,X.H.,Chen,Y.,Li,J.,Yang,C.,Ling,X.X.,Tchouankoue,J.P.,2016.NewisotopicconstraintsonageandoriginofMesoarcheancharnockite,trondhjemiteandamphiboliteintheNtemComplexofNWCongoCraton,southernCameroon.PrecambrianResearch,276,14–23. 19.Liu,C.Z.,Chung,S.L.,Wu,F.Y.,Zhang,C.,Xu,Y.,Wang,J.G.,Chen,Y.,Guo,S.,2016.TethyansuturinginSoutheastAsia:ZirconU-PbandHf-OisotopicconstraintsfromMyanmarophiolites.Geology,44,311–318. 18.Guo,S.,Chen,Y.,Liu,C.Z.,Wang,J.G.,Su,B.,Gao,Y.J.,Wu,F.Y.,Sein,K.,Yang,Y.H.,Mao,Q.,2016.ScheeliteandcoexistingF-richzonedgarnet,vesuvianite,fluorite,andapatiteincalc-silicaterocksfromtheMogokmetamorphicbelt,Myanmar:ImplicationsformetasomatisminmarbleandtheroleofhalogensinWmobilizationandmineralization.JournalofAsianEarthSciences,117,82–106. 17.Guo,S.,Chen,Y.,Ye,K.,Su,B.,Yang,Y.H.,Zhang,L.M.,Liu,J.B.,Mao,Q.,2015.Formationofmultiplehigh-pressureveinsinultrahigh-pressureeclogite(Hualiangting,Dabieterrane,China):Fluidsource,elementtransfer,andclosed-systemmetamorphicveining.ChemicalGeology,417,238–260. 16.Liu,S.A.,Huang,J.,Liu,J.G.,Woerner,G.,Yang,W.,Tang,Y.J.,Chen,Y.,Tang,L.M.,Zheng,J.P.,Li,S.G.,2015.CopperisotopiccompositionofthesilicateEarth.EarthandPlanetaryScienceLetters,427,95–103. 15.Guo,S.,Ye,K.,Cheng,N.F.,Chen,Y.,Su,B.,Liu,J.B.,2015.MetamorphicP-Ttrajectoryandmulti-stagefluideventsofvein-bearingUHPeclogitesfromtheDabieterrane:insightsfromcompositionalzonationsofkeyminerals.InternationalGeologyReview,57,1077–1102. 14.Liu,P.L.,Wu,Y.,Chen,Y.,Zhang,J.F.,Jin,Z.M.,2014.UHPimpuremarblesfromtheDabieMountains:Metamorphicevolutionandcarboncyclingincontinentalsubductionzones.Lithos,212,280–297. 13.Xiao,L.L.,Liu,F.L.,Chen,Y.,2014.MetamorphicP-T-tpathsoftheZanhuangmetamorphiccomplex:ImplicationsforthePaleoproterozoicevolutionoftheTrans-NorthChinaOrogen.PrecambrianResearch,255,216–235. 12.Guo,S.,Ye,K.,Yang,Y.H.,Chen,Y.,Zhang,L.M.,Liu,J.B.,Mao,Q.,Ma,Y.G.,2014.InsituSrisotopicanalysesofepidote:tracingthesourcesofmulti-stagefluidsinultrahigh-pressureeclogite(Ganghe,Dabieterrane).ContributionstoMineralogyandPetrology,167,DOI:10.1007/s00410-014-0975-9. 11.GuoS.,YeK.,WuT.F.,ChenY.,YangY.H.,ZhangL.M.,LiuJ.B.,MaoQ.,MaY.G.,2013.Apotentialmethodtoconfirmthepreviousexistenceoflawsoniteineclogite:themassimbalanceofSrandLREEsinmultistageepidote(Ganghe,DabieUHPterrane),JournalofMetamorphicGeology,31(4),415–435. 10.Xu,H.J.,Ye,K.,Song,Y.R.,Chen,Y.,Zhang,J.F.,Liu,Q.,Guo,S.,2013.Progrademetamorphism,decompressionalpartialmeltingandsubsequentmeltfractionalcrystallizationintheWeihaimigmatiticgneisses,Sulu.ChemicalGeology,341,16–37. 9.郭顺,叶凯,陈意,刘景波,毛骞,2013。大别山榴辉岩中超高压硬柱石脱水分解及其对俯冲带深部流体活动的制约。科学通报,58(22):2186–2191。 8.刘景波,张灵敏,陈意,郭顺,程南飞,2013。大别-苏鲁造山带超高压榴辉岩和脉体磷灰石含氯特征与变质流体演化。科学通报,58(22):2165–2168. 7.郭顺,叶凯,陈意,刘景波,张灵敏,2013。开放地质体系中物质迁移质量平衡计算方法介绍。岩石学报,29,1486–1498. 6.张灵敏,刘景波,程南飞,叶凯,郭顺,陈意,毛骞,2013。大别-苏鲁高压-超高压变质带榴辉岩和脉体中磷灰石氯含量和流体盐度关系的研究。岩石学报,29,1525–1539. 5.Guo,J.H.,Peng,P.,Chen,Y.,Jiao,S.J.,Windley,B.F.,2012.UHTsapphirinegranulitemetamorphismat1.93-1.92Gacausedbygabbronoriteintrusions:ImplicationsfortectonicevolutionofthenorthernmarginoftheNorthChinaCraton.PrecambrianResearch,222,124–142. 4.Guo,S.,Ye,K.,Chen,Y.,Liu,J.B.,Mao,Q.,Ma,Y.G.,2012.Fluid-rockinteractionandelementmobilizationinUHPmetabasalt:Constraintsfromanomphacite-epidoteveinandhosteclogitesintheDabieorogen.Lithos,136,145–167. 3.Ye,K.,Song,Y.R.,Chen,Y.,Xu,H.J.,Liu,J.B.,Sun,M.,2009.Multistagemetamorphismoforogenicgarnet-lherzolitefromZhimafang,SuluUHPterrane,E.China:Implicationsformantlewedgeconvectionduringprogressiveoceanicandcontinentalsubduction.Lithos,109,155–175. 2.Guo,S.,Ye,K.,Chen,Y.,Liu,J.B.,2009.Anormalizationsolutiontomasstransferillustrationofmultipleprogressivelyalteredsamplesusingtheisocondiagram.EconomicGeology,104,881–886. 1.Sun,M.,Chen,N.S.,Zhao,G.C.,Wilde,S.A.,Ye,K.,Guo,J.H.,Chen,Y.,Yuan,C.,2008.U-PbzirconandSm-NdisotopicstudyoftheHuangtulinggranulite,Dabie-Sulubelt,China:ImplicationforthepaleoproterozoictectonichistoryoftheYangtzeCraton.AmericanJournalofScience,308,469–483.

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