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2018.
1.ChenJ.L.*,YinA.*,XuJ.F.,DongY.H.,KangZ.Q.2018.LateCenozoicmagmaticinflation,crustalthickening,and>2kmofsurfaceupliftincentralTibet.Geology,46:19-22.
2.ZengY.C.,XuJ.F.,ChenJ.L.*,WangB.D.,HuangF.,YuH.X.,ChenX.F.,ZhaoP.P.,2018.BreakupofEasternGondwanaasinferredfromtheLowerCretaceousCharongDoleritesinthecentralTethyanHimalaya,southernTibet.Palaeogeography,Palaeoclimatology,Palaeoecology,doi.org/10.1016/j.palaeo.2017.10.010.
3.ZengY.C.,XuJ.F.,ChenJ.L.,WangB.D.,KangZ.Q.,HuangF.,2018.GeochronologicalandgeochemicalconstraintsontheoriginoftheYunzhugophioliteintheShiquanhe–Yunzhug–NamuTsoophiolitebelt,LhasaTerrane,TibetanPlateau.Lithos,300-301:250-260.
4.ZengY.C.,ChenQ.,XuJ.F.,ChenJ.L.,HuangF.,YuH.X.,ZhaoP.P.,2018.PetrogenesisandgeodynamicsignificanceofNeoproterozoic(~925Ma)high-Fe–TigabbrosoftheRenTsoophiolite,LhasaTerrane,centralTibet.PrecambrianResearch,,314:160-169
5.ZhangH.R.,ChenJ.L.,YangT.N.,HouZ.Q.,AghazadehM.,2018.JurassicgranitoidsinthenorthwesternSanandaj–SirjanZone:EvolvingmagmatisminresponsetothedevelopmentofaNeo-Tethyanslabwindow.GondwanaResearch.https://doi.org/10.1016/j.gr.2018.01.012.
6.YangT.N,ChenJ.L.,LiangM.J.,XinD.,AghazadehM.,HouZ.Q.,ZhangH.R.,2018.TwoplutoniccomplexesoftheSanandaj-Sirjanmagmatic-metamorphicbeltrecordJurassictoEarlyCretaceoussubductionofanoldNeotethysbeneaththeIranmicroplate.GondwanaResearch,https://doi.org/10.1016/j.gr.2018.03.016.
7.谈荣钰,陈建林*,许继峰,黄文龙,唐婉丽,2018.跨越中甸弧到扬子地块西缘的~80Ma中酸性火成岩成因及其对碰撞后成矿的意义.岩石学报,34(5):1413-1426.
8.唐婉丽,许继峰,陈建林*,谈荣钰,黄文龙,2018.滇西腾冲地区滇滩A型花岗岩的年代学、地球化学及其构造意义.地球化学,47(1):1-13.
2017.
1.ChenJ.L.*,XuJ.F.,RenJ.B.,HuangX.X.,2017.LateTriassicE-MORB-likebasaltsassociatedwithporphyryCu-depositsinthesouthernYiduncontinentalarc,easternTibet:Evidenceofslab-tearduringsubduction?OreGeologyReview,90:1054-1062.
2.ZengY.C.,ChenJ.L.*,XuJ.F.,LaiM.,XiongQ.W.,2017.OriginofMioceneCu-bearingporphyriesintheZhunuoregionofthesouthernLhasasubterrane:constraintsfromgeochronologyandgeochemistry.GondwanaResearch,41:51-64.
3.HuangF.,XuJ.F.,LiuY.S.,LiJ.,ChenJ.L.,LiX.Y.,2017.Re–OsisotopeevidencefromMesozoicandCenozoicbasaltsforsecularevolutionofthemantlebeneaththeNorthChinaCraton.ContributionstoMineralogyandPetrology,172:28.
4.HuangF.,Xu,J.F.,ZengYC.,ChenJ.L.,WangB.D.,YuH.X.,ChenL.,HuangW.L.,TangR.U.,2017.SlabBreakoffoftheNeo-TethysOceanintheLhasaTerraneInferredFromContemporaneousMeltingoftheMantleandCrust.Geochemistry,Geophysics,Geosystems,18:4074-4095.
5.WangB.D.,WangL.Q.,ChenJ.L.,LiuH.,YinF.G.,LiX.B.,2017.PetrogenesisofLateDevonian–EarlyCarboniferousvolcanicrocksinnorthernTibet:NewconstraintsonthePaleozoictectonicevolutionoftheTethyanOcean.GondwanaResearch,41:142-156.
6.HuangT.T.,XuJ.F.,ChenJ.L.,WuJ.B.,ZengY.C.,2017.SedimentaryrecordofJurassicnorthwardsubductionoftheBangong–NujiangOcean:insightsfromdetritalzircons.InternationalGeologyReview,59(2):166-184.
7.冉孟兰,康志强,许继峰,付文春,杨锋,王保弟,陈建林,李强,付伟.2017.西藏拉萨地块南缘日喀则地区比马组火山岩的年代学、地球化学及其地质意义.地球化学,46(3):205-218.
2016.
1.ZengY.C.,ChenJ.L.,XuJ.F.,WangB.D.,HuangF.,2016.Sedimentmeltingduringsubductioninitiation:GeochronologicalandgeochemicalevidencefromtheDarutsohigh-Mgandesiteswithinophiolitemelange,centralTibet.Geochemistry,Geophysics,Geosystems,doi:10.1002/2016GC006456.
2.CaoK.,XuJ.F.,ChenJ.L.*,HuangX.X.,RenJ.B.,ZhaoX.D.,LiuZ.X.,2016.Double-layerstructureofthecrustbeneaththeZhongdianarc,SWChina:U-PbgeochronologyandHfisotopeevidence.JournalofAsianEarthScience,115:455-467.
3.KongD.X.,Xu,J.F.,Chen,J.L*.2016.Oxygenisotopeandtraceelementgeochemistryofzirconsfromporphyrycoppersystem:ImplicationsforLateTriassicmetallogenesiswithintheYidunTerrane,southeasternTibetanPlateau.ChemicalGeology,441,148-161.
4.WangB.D.,WangL.Q.,ChungS.L.,ChenJ.L.,YinF.G.,LiuH.,LiX.B.,ChenL.K.,2016.EvolutionoftheBangong–NujiangTethyanocean:Insightsfromthegeochronologyandgeochemistryofmaficrockswithinophiolites.Lithos,245:18-33.
5.HuangF.,XuJ.F.,ChenJ.L.,WuJ.B.,ZengY.C.,XiongQ.W.,ChenX.F.,YuH.X.2016.TwoCenozoictectoniceventsofN-SandE-WextensionintheLhasaterrane:evidencefromgeologyandgeochronology.Lithos,245:118-132.
6.黄文龙,许继峰,陈建林,黄丰,曾云川,皮桥辉,蔡永丰,蒋兴洲.2016.云南个旧杂岩体年代学与地球化学:岩石成因和幔源岩浆对锡成矿贡献.岩石学报,32(8):2330-2346.
2015
1.HuangF.,ChenJ.L.,XuJ.F.,WangB.D.,LiJ.,2015.Os-Nd-SrisotopesinMioceneultrapotassicrocksofsouthernTibet:Partialmeltingofapyroxenite-bearinglithosphericmantle?GeochimicaetCosmochimicaActa,163:279-298.
2.ChenJ.L.*,XuJ.F.,YuH.X.,WuJ.B.,WangB.D.,FengY.X.,2015.LateCretaceoushigh-Mg#granitoidsinsouthernTibet:implicationsforearlycrustalthickeningandtectonicevolutionoftheTibetanplateau?Lithos,232:12-22.
3.ChenJ.L.*,XuJ.F.,WangB.D.,YangZ.M.,RenJ.B.,YuH.X.,LiuH.F.,FengY.X.,2015.Geochemicaldifferencesbetweensubduction-andcollision-relatedcopper-bearingporphyriesandimplicationsformetallogenesis.OreGeologyReview,70:424-437.
4.KongD.X.,XuJ.F.,YinJ.F.,ChenJ.L.,LiJ.,GuoY.,YangH.T.,ShaoX.K.,2015.ElectronmicroprobeanalysesoforemineralsandH-O,SisotopegeochemistryoftheYueryagolddeposit,easternHebei,China:implicationsfororegenesisandmineralization.OreGeologyReview,69:199-216.
5.黄丰,许继峰,陈建林,康志强,董彦辉.2015.早侏罗世叶巴组与桑日群火山岩:特提斯洋俯冲过程中的陆缘弧与洋内弧?岩石学报,31:2089-2900.
6.雷鸣,陈建林*,许继峰,曾云川.2015.拉萨地块中北部尕尔穷晚白垩世早期高镁闪长玢岩地球化学特征指示:加厚下地壳的拆沉?地质通报,34:337-346.
7.熊秋伟,陈建林*,许继峰,黄丰,陈雪峰,曾云川,雷鸣.2015.拉萨地块南部得明顶地区叶巴组火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其成因.地质通报,34:1645-1655.
2014
1.ChenJ.L.*,XuJ.F.,RenJ.B.,HuangX.X.,WangB.D.,2014.GeochronologyandgeochemicalcharacteristicsofLateTriassicporphyriticrocksfromtheZhongdianarc,easternTibet,andtheirtectonicandmetallogenicimplications.http://10.20.40.10/webpic/W0201808/W020180804/W020180804361410802083.gifGondwanaResearch.26:492-504.
2.WangB.D.,ChenJ.L.*,XuJ.F.,WangL.Q.,2014.GeochemicalandSr-Nd-Pb-OsisotopiccompositionsofMioceneultrapotassicrocksinsouthernTibet:petrogenesisandimplicationsfortheregionaltectonichistory.Lithos,208-209:237-250.
3.WangB.D.,WangL.Q.,ChenJ.L.,YinF.G.,WangD.B.,ZhangW.P.,ChenL.K.,LiuH.,2014.Triassicthree–stagecollisioninthePaleo–Tethys:ConstraintsfrommagmatismintheJiangda–Deqen–Weixicontinentalmarginarc,SWChina.GondwanaResearch,26:457-491.
4.KangZ.Q.,XuJ.F.,WildeS.A.,FengZ.H.,ChenJ.L.,WangB.D.,FuaW.C.,PanH.B.2014.GeochronologyandgeochemistryoftheSangriGroupVolcanicRocks,SouthernLhasaTerrane:ImplicationsfortheearlysubductionhistoryoftheNeo-TethysandGangdeseMagmaticArc.Lithos,200-201:157-168.
5曹康,许继峰,陈建林,黄肖潇,任江波,2014.云南普朗超大型斑岩铜矿床含矿斑岩成因及其成矿意义.矿床地质,33:307-322.
6.许继峰,邬建斌,王强,陈建林,曹康.2014.埃达克岩与埃达克质岩在中国的研究进展.矿物岩石地球化学通报,33:6-13.
2013
1.ChenJ.L.*,XuJ.F.,DongY.H.,WangB.D.,KangZ.Q.2013.GeochemistryofEoceneHhigh-Mg#adakiticrocksinthenorthernQiangtangterrane,centralTibet:implicationsforearlydelaminationoflowercrustalandearlyupliftingofincentertheplateau?GeologicalSocietyofAmericaBulletin,125(11-12):1800-1819.
2.王保弟,许继峰,刘保民,陈建林,王立全,郭琳,王冬兵,张万平.2013.拉萨地块北部~90Ma斑岩型矿床年代学及成矿地质背景.地质学报,87:71-80.
3.陈玲,许继峰,陈建林,任江波,黄肖潇.2013.云南中甸地区翁水晚三叠世火山岩地球化学特征及其构造意义.岩石学报,29(4):1156-1166.
4.呼建雄,陈建林*,张占武,姚胜,王贝,杨文,许继峰,邬建斌,黄丰,曾云川.2013.青藏高原南部谢通门侏罗纪埃达克质岩地球化学特征及其形成机制.大地构造与成矿,37(2):320-332.
2012.
1.ChenJ.L.*,ZhaoW.X.,XuJ.F.,WangB.D.,KangZ.Q.2012.GeochemistryofMiocenetrachytesinBugasi,Lhasablock,TibetanPlateau:Mixingproductsbetweenmantle-andcrust-derivedmelts?http://10.20.40.10/webpic/W0201808/W020180804/W020180804361410802083.gifGondwanaResearch,21:112-122.
2.ChenJ.L.*,XuJ.F.,WangB.D.,KangZ.Q.2012.GeochemicalcomparisonsofCenozoicMgO-richpotassicrocksinthesouthernandNorthernTibetanPlateau:heterogeneityofsubcontinentallithosphericmantleandtectonicimplications.JournalofAsianEarthSciences,53:115-130.
3.黄肖潇,许继峰,陈建林,任江波.2012.中甸岛弧红山地区两期中酸性侵入岩的年代学、地球化学特征及其成因.岩石学报,28(5):1493-1506.
4.郭倩,赵文霞,陈建林,王保弟.2012.西藏松多榴辉岩矿物出溶体研究.岩石学报,28(5):1689-1696.
5.于丽芳,赵文霞,陈建林,郭倩,王保弟.2012.西藏当惹雍错富钾和富钠碱性火山岩的矿物学研究及其成因指示.大地构造与成矿,36(2):274-283.
2011.
1.ChenJ.L.,XuJ.F.,ZhaoW.X.,DongY.H.,WangB.D.,KangZ.Q.2011.GeochemicalvariationsinMioceneadakiticrocksfromthewesternandeasternLhasaterrane:ImplicationsforlowercrustalflowbeneaththeSouthernTibetanPlateau.Lithos,125:928-939.
2.陈建林,许继峰,任江波,王保弟,余红霞.2011.俯冲型和碰撞型含矿斑岩地球化学组成的差异.岩石学报,27(9):2733-2742.
3.余红霞,陈建林*,许继峰,王保弟,邬建斌,梁华英.2011.拉萨地块中北部晚白垩世(约90Ma)拨拉扎含矿斑岩地球化学特征及其成因.岩石学报,27(7):2011-2022.
4.赵文霞,于丽芳,陈建林,郭倩,王保弟.2011.青藏米巴勒地区中新世钠质方沸石(霞石)响岩中单斜辉石环带研究:对岩浆-构造演化的启示.岩石学报,27(7):2073-2082.
5.于丽芳,赵文霞,陈建林,郭倩,王保弟.2011.拉萨地块中南部新生代超钾质岩中单斜辉石斑晶的环带成分研究.岩石学报,27(12):3666-3674.
6.任江波,许继峰,陈建林.2011.中甸岛弧成矿斑岩的锆石年代学及其意义.岩石学报,27(9):2591-2599.
7.王保弟,陈陵康,许继峰,刘鸿飞,陈建林,康志强.2011.拉萨地块麻江地区具有“超钾质”成分的钾质火山岩的识别及成因讨论.岩石学报,27(6):1662-1674.
8.任江波,许继峰,陈建林,张世权,梁华英.2011.“三江”地区中甸弧普朗斑岩地球化学特征及其成因.岩石矿物学杂志,30(4):581-592.
2010.
1.ChenJ.L.,XuJ.F.,WangB.D.,KangZ.Q.2010.OriginofCenozoicalklinepotassicvolcanicrocksatKonglongxiang,Lhasaterrane,TibetanPlateau:productsofpartialmeltingofmaficlower-crustalsource?ChemicalGeology,273:286-299.
2.ChenJ.L.,XuJ.F.,WangB.D.,KangZ.Q.2010.GeochemistryoftheEoceneFelsicPorphyricRocksandHigh-MgPotassicRocksalongJARSZ:ImplicationfortheTectonicEvolutioninEasternTibet.ActaGeologicaSinica,84(6):1448-1460.
3.WangB.D.,ChenJ.L.,XuJ.F.,etal.2010.ChronologyandGeochemistryoftheNadingcuoVolcanicRocksintheSouthernQiangtangRegionoftheTibetanPlateau:PartialMeltingofRemnantOceanCrustalongtheBangong-NujiangSuture.ActaGeologicaSinica,84(6):1461-1473.
4.陈建林,许继峰,王保弟,康志强.2010.“三江”地区与青藏高原内部早第三纪高镁钾质岩地球化学对比:地幔源区的差异及其意义.岩石学报,26(6):1856-1870.
5.陈建林,许继峰,王保弟,康志强.2010.青藏高原拉萨地块新生代超钾质岩与南北向地堑成因关系.岩石矿物学杂志,29(4):341-354.
6.王保弟,许继峰,陈建林,张兴国,王立全,夏抱本.2010.冈底斯东段汤不拉斑岩Mo-Cu矿床成岩成矿时代与成因关系.岩石学报,26(6):1820-1832.
7.康志强,许继峰,王保弟,陈建林.2010.拉萨地块北部去申拉组火山岩:班公湖-怒江特提斯洋南向俯冲的产物?.岩石学报,26(10):3106-3116.
8.康志强,许继峰,陈建林,王保弟,董彦辉.2010.西藏南部桑日群火山岩的时代:来自晚期马门侵入体的约束.地球化学,39(6):1-11.
9.许继峰,王桂琴,李杰,陈建林.2010.月球物质的Re-Os同位素组成研究:对月球后期增生历史的指示.地球化学,39(2):142-148.
2009~2005
1.ChenJ.L.,XuJ.F.,WangB.D.,etal.2009.MultistageandheterogeneousupliftoftheTibetanPlateauimplicatedbythemulti-episodepost-collisionlava.GCA,A212.
2.陈建林,许继峰,康志强,王保弟.2008.青藏高原南部与北部新生代高镁钾质岩地球化学对比:南北地幔源区成分差异.岩石学报,24(2):211-224.
3.陈建林,许继峰,康志强,王保弟.2007.青藏高原西南部查孜地区中新世钾质火山岩地球化学研究及其成因.地球化学,36(5):437-447.2007.
4.陈建林,许继峰,康志强,王保弟.2006.青藏高原西部措勤县地区中新世布嘎寺组钾质火山岩成因.岩石学报,22(3):585-594.
5.http://10.20.40.10/webpic/W0201808/W020180804/W020180804361410802083.gif康志强,许继峰,陈建林,王保弟.2009.藏南白垩纪桑日群麻木下组埃达克岩的地球化学特征及其成因.地球化学,38(4):334-344.
6.康志强,许继峰,王保弟,董彦辉,王树庆,陈建林.2009.拉萨地块北部白垩纪多尼组火山岩的地球化学:形成的构造环境.地球科学-中国地质大学学报,34(1):89-104.
7.王保弟,许继峰,张兴国,陈建林,康志强,董彦辉.2008.青藏高原西部赛利普中新世火山岩源区:地球化学及Sr-Nd同位素制约.岩石学报,24(2):265-278.
8.王保弟,许继峰,曾庆高,康志强,陈建林,董彦辉.2007.西藏改则地区拉果错蛇绿岩地球化学特征及成因.岩石学报,23(6):1521-1530
9.王金荣,郭原生,付善明,陈建林,等.2005.甘肃黑石山早古生代埃达克质岩的发现及其构造动力学意义.岩石学报,21(3):997-985.