蔡春芳
近期热点
资料介绍
个人简历
蔡春芳,1966年生于福建省福清市。现为长江大学地环学院楚天学者特聘教授、中科院地质与地球物理研究所研究员、博士生导师、国家杰出青年基金获得者。于1987、1990年分别获江汉石油学院学士和硕士学位;2000年获得中科院地质与地球物理所博士学位。主要从事塔里木、四川、鄂尔多斯盆地储层/油藏流体(石油、天然气与地层水)与岩石之间相互作用(微生物与热化学硫酸盐作用TSR),以及应用有机硫同位素,来探讨高过成熟烃源岩—油气对比。给出证据显示最稳定的甲烷可以是TSR的主要反应物、阐明了其碳同位素分馏效应,提出TSR过程新产生了硫醇、噻吩和四氢噻吩等有机含硫化合物,研发了烃源岩有机硫含量和同位素测试方法,发现在快速埋藏的盆地中,可以应用未受次生改造的原油及其二苯并噻吩的硫同位素值来进行油—源对比,论证了塔里木盆地塔中古生界发生了穿层的热卤水流动,阐明原油来自寒武系,提出深埋白云岩优质储层形成于早期白云石化和后期TSR导致的硬石膏、白云石溶解作用;发现了铀矿硫酸盐还原细菌成因的微化石、硫和碳同位素证据,阐明其成矿模式;认为寒武纪生物大爆发与深海表层氧化水体扩大有关。发表第一作者国际SCI论文18篇,三篇被SCI引文>65次,最高116次,H-index为14,在国内同行中名列前茅。指导毕业了7名博士、硕博连读研究生(李洪涛、李开开、向雷、姜磊、贺训云、贾连奇、袁余洋)、1名硕士研究生(蔡蹓璐)。这些学生大多在国际著名刊物以第一作者发表了论文。合作指导博士后4人(姜红霞、李开开、姜磊、贾连奇)、博士生(刘玲)、硕士生2人(陈坤、陈双玲)。研究领域
1)沉积盆地不同存在形式硫之间转化及其机理2)有机硫/碳氮同位素应用于恢复古环境、生命演化以及高过成熟烃源岩-油气的对比研究;3)碳酸盐岩中TSR及其他流体—岩石相互作用对有效储层形成与改造机理与油气成藏作用的关系;4)深埋成岩期,BSR与TSR成因的硫化物形成有机含硫化合物的机理及其识别;5)硫酸盐还原菌降解油气与六价铀还原成矿的关系;6)生物标志化合物、稳定同位素和流体包裹体在油气勘探和开发中的应用。"主持/主要参加的科研项目1.塔中地区奥陶系硫化氢成因与分布。油田横向课题,2012.10-2014.062.油气盆地硫参与的有机—无机相互作用近期论文
2015年Cai,C.F.,Hu,G.Y.,Li,H.X.,Jiang,L.,He,W.X.,Zhang,B.S.,Jia,L.Q.,Wang,T.K.OriginsandfatesofH2SintheCambrianandOrdovicianinTazhongarea:evidencefromsulfurisotopes,fluidinclusionsandproductiondata.MarineandPetroleumGeology,2015c,67,408-418.Cai,C.F.,Zhang,C.M.,Worden,R.H.,Wang,T.K.,Li,H.X.,Jiang,L.,HuangS.Y.,Zhang,B.S.Applicationofsulfurandcarbonisotopestooil–sourcerockcorrelation:AcasestudyfromtheTazhongarea,TarimBasin,China.OrganicGeochemistry,2015b,83-84,140-152.Cai,C.F.,Xiang,L.,Yuan,Y.Y.,He,X.Y.,Chu,X.L.,Chen,Y.,Xu,C.L.MarineC,SandNbiogeochemicalprocessesintheredox-stratifiedEarlyCambrianYangtzeocean.JournaloftheGeologicalSociety(London).2015a,172(3),390-406.Jiang,L.,Cai,C.F.,Worden,R.H.,Li,K.K.,Xiang,L.,Chu,X.L.,Shen,A.J.,Li,W.J.Rareearthelementandyttrium(REY)geochemistryincarbonatereservoirsduringdeepburialdiagenesis:ImplicationsforREYmobilityduringthermochemicalsulfatereduction.ChemicalGeology,2015,415,87–101.Jiang,L.,Worden,R.H.,Cai,C.F.Generationofisotopicallyandcompositionallydistinctwaterduringthermochemicalsulfatereduction(TSR)incarbonatereservoirs:TriassicFeixianguanFormation,SichuanBasin,China.GeochimicaetCosmochimicaActa,2015,169,249-262.Jiang,L.,Pan,W.,Cai,C.F.,Jia,L.Q.,Pan,L.,Wang,T.K.,Li,H.X.,Chen,S.L.,Chen,Y.FluidmixinginducedbyhydrothermalactivityintheordoviciancarbonatesinTarimBasin,China.Geofluids,2015,169,249-262.Jia,L.Q.,Cai,C.F.,Yang,H.,Li,H.X.,Wang,T.,Zhang,B.,Jiang,L.,Tao,X.W.ThermochemicalandbacterialsulfatereductionintheCambrianandLowerOrdoviciancarbonatesintheTazhongArea,TarimBasin,NWChina:Evidencefromfluidinclusions,C,SandSrisotopicdata.Geofluids,2015,15,421–437.2014年Wang,Z.M.,Cai,C.F.,Li,H.X.,Yang,H.J.,Wang,T.K.,Zhang,K.,Jia,L.Q.,Chen,K.OriginoflatechargedgasanditseffectonpropertyofoilsintheOrdovicianinTazhongarea.JournalofPetroleumScienceandEngineering,2014,122,83-93.Cai,C.F.,He,W.X.,Jiang,L.,Li,K.K.,Xiang,L.,Jia,L.Q.PetrologicalandgeochemicalconstraintsonporositydifferencebetweenLowerTriassicsour-andsweet-gascarbonatereservoirsintheSichuanBasin.MarineandPetroleumGeology,2014,56,34-50.Jiang,L.,Worden,R.H.,Cai,C.F.,Li,K.K.,Xiang,L.,Cai,L.L.,He,X.Y.Dolomitizationofgasreservoirs:theUpperPermianChangxingandLowerTriassicFeixianguanFormations,northeastSichuanBasin,China.JournalofSedimentaryResearch,2014,84,792-815.Jiang,L.,Worden,R.H.,Cai,C.F.ThermochemicalsulfatereductionandfluidevolutionoftheLowerTriassicFeixianguanFormationsourgasreservoirs:NortheastSichuanBasin,China,AmericanAssociationofPetroleumGeologistsBulletin,2014,98,947-973.Li,K.K.,Cai,C.F.,Hou,D.J.,He,X.Y.,Jiang.L.,Jia,L.Q.,Cai,L.L.,2014.OriginofhighH2SconcentrationsintheUpperPermianChangxingreservoirsoftheNortheastSichuanBasin,China.MarineandPetroleumGeology57,233-243.Li,K.K.,Cai,C.F.,Jia,L.Q.,Gao,Y.,Jiang,Z.,Wang,T.K.,Jiang,L.,2014.Theroleofthermochemicalsulfatereductioninthegenesisofhigh-qualitydeepmarinereservoirswithinthecentralTarimBasin,westernChina.ArabianJournalofGeosciences,1-14.Yuan,Y.Y.,Cai,C.F.,Wang,T.K.,Xiang,L.,Jia,L.Q.,Chen,Y.,2014.Deep-waterbasinredoxconditionsduringEdiacaran-CambriantransitionperiodintheLowerYangtze,SouthChina:Casestudyofironspeciationandδ13CorginDibenSection,Zhejiangprovince.ChineseScienceBulletin,72,1-139.2013年Cai,C.F.,Zhang,C.M.,He,H.,Tang,Y.J.,2013.Carbonisotopefractionationduringmethane-dominatedTSRinEastSichuanBasingasfields,China:Areview.MarineandPetroleumGeology48,100-110.Jiang,L.,Cai,C.F.,Worden,R.H.,Li,K.K.,Xiang,L.,2013.RefluxdolomitizationoftheUpperPermianChangxingFormationandtheLowerTriassicFeixianguanFormation,NESichuanBasin,China.Geofluids13,232-245.贺训云,蔡春芳,姚根顺,熊湘华,沈安江,向雷,吴敬武,2013.黔南坳陷油苗来源:碳,硫同位素及生物标志物证据.岩石学报29(3):1059-1072.2012年Li,K.K.,Cai,C.F.,Jiang,L.,Cai,L.L.,Jia,L.Q.,Zhang,B.,Xiang,L.,Yuan,Y.Y.,2012.SrevolutionintheUpperPermianandLowerTriassiccarbonates,NortheastSichuanBasin,China:constraintsfromchemistry,isotopeandfluidinclusions.AppliedGeochemistry27,2409-2424.Jiang,L.,Cai,C.F.,Zhang,Y.D.,Mao,S.Y.,Sun,Y.G.,Li,K.K.,Xiang,L.,Zhang,C.M.,2012.Lipidsofsulfate-reducingbacteriaandsulfur-oxidizingbacteriafoundintheDongshenguraniumdeposit.ChineseScienceBulletin57,1311-1319.蔡春芳,蔡镠璐,张俊,蔡勋育,李开开,2012.川东北飞仙关组甲烷为主的TSR及其同位素分馏作用.岩石学报28(3):889-894.李开开,蔡春芳,蔡镏璐,姜磊,向雷,2012.塔河地区中下奥陶统储层硫化物成因分析.岩石学报28(3):806-814.向雷,蔡春芳,贺训云,姜磊,2012.贵州渣拉沟剖面下寒武统黑色硅质岩微量元素富集机制.岩石学报28(3):971-980.杨海军,李开开,潘文庆,肖中尧,蔡春芳,2012.塔中地区奥陶系埋藏热液溶蚀流体活动及其对深部储层的改造作用.岩石学报28(3):783-792.张俊,蔡镠璐,向雷,蔡春芳,2012.川东北地区飞仙关组成岩晚期白云石溶解作用.石油与天然气地质33(4):599-606.2011年Li,K.K.,Cai,C.F.,He,H.,Jiang,L.,Cai,L.L.,Xiang,L.,Huang,S.J.,Zhang,C.M.,2011.Originofpalaeo-watersintheOrdoviciancarbonatesinTaheoilfield,TarimBasin:constraintsfromfluidinclusionsandSr,CandOisotopes.Geofluids11,71-86.Zhang,C.M.,Zhang,Y.Q.,Cai,C.F.,2011.Maturityeffectoncarbazoledistributionsinsourcerocksfromthesalinelacustrinesettings,thewesternQaidamBasin,NWChina.JournalofAsianEarthSciences42,1288-1296.Zhang,C.M.,Zhang,Y.Q.,Cai,C.F.,2011.Aromaticisoprenoidsfromthe25-65MasalinelacustrineformationsinthewesternQaidamBasin,NWChina.OrganicGeochemistry42,851-855.2010年Cai,C.F.,Li,K.K.,Zhu,Y.M.,Xiang,L.,Jiang,L.,Tenger,Cai,X.Y.,Cai,L.L.,2010.TSRoriginofsulfurinthePermianandTriassicreservoirbitumeninEastSichuanBasin,China.OrganicGeochemistry41,871-878.2009年Cai,C.F.,Zhang,C.M.,Cai,L.L.,Wu,G.H.,Jiang,L.,Xu,Z.M.,Li,K.K.,Ma,A.L.,Chen,L.X.,2009c.OriginsofPalaeozoicoilsintheTarimBasin:Evidencefromsulfurisotopesandbiomarkers.ChemicalGeology268,197-210.蔡春芳,李开开,李斌,蔡镠璐,姜磊,2009b.塔河地区奥陶系碳酸盐岩缝洞充填物的地球化学特征及其形成流体分析.岩石学报25(10),2399-2404.Cai,C.F.,LiKK.,Ma,A.L.,Zhang,C.M.,Xu,Z.M.,Worden,R.H.,Wu,G.H.,Zhang,B.S.,Chen,L.X.,2009a.DistinguishingCambrianfromUpperOrdoviciansourcerocks:EvidencefromsulfurisotopesandbiomarkersintheTarimBasin.OrganicGeochemistry40,755-768.Cai,C.F.,LiKK.,Jiang,L.,Cai,L.L.2009.ReservoirporosityenhancementbymultiplestagesofTSRinEastSichuanBasingasfields,China.GeochimicaCosmochimiActa73,Axxx.2008年Cai,C.F.,Li,KK,Li,H.T.,Zhang,B.S.,2008.Evidenceforcrossformationalhotbrineflowfromintegrated87Sr/86Sr,REEandfluidinclusionsoftheOrdovicianveinsinCentralTarim.AppliedGeochemistry23,2226-2235.Cai,C.F.,LiKK.,2008.SecularchangeindeltaS-34valueofearlypalaeozoickerogensfromtheTarimBasinrelativetomarinesulphates.GeochimicaCosmochimiActa72(12),A128.蔡春芳,李宏涛,李开开,姜磊,2008.油气厌氧氧化与铀还原的耦合关系-以东胜和钱家店铀矿床为例。石油实验地质,30(5),518-521.李开开,蔡春芳,蔡镠鏴,2008.塔中地区上奥陶统热液流体与热化学硫酸盐还原作用.石油与天然气地质,2(29):217-222ZhangCM,ZhangYQ,ZhangM,ChenZY,PengDH,SunWL,Cai,C.F.,2008.CompositionalvariabilitiesamongcrudeoilsfromthesouthwesternpartoftheQaidamBasin,NWChina.JournalofPetroleumScienceandEngineering62,87-92.ZhangCM,ZhangYQ,ZhangM,ZhaoHJ,Cai,C.F.,2008.Carbazoledistributionsinrocksfromnon-marinedepositionalenvironments.OrganicGeochemistry39,868-878.JiangHX,WuYS,Cai,C.F.,2008.FilamentouscyanobacteriafossilsandtheirsignificanceinthePermian-TriassicboundarysectionatLaolongdong,Chongqing.ChineseScienceBulletin53,1871-1879.2007年Cai,C.F.,Li,KK,Li,H.T.,2007.Evidenceforcrossformationhotbrineflowfromintegrated87Sr/86SrandREEdatainCentralTarim.GeochimicaCosmochimiActaA139-A139(SCI).Cai,C.F.,Li,KK,Li,H.T.,2007.FluidinclusionandisotopicconstraintforfluidevolutionintheOrdovicianveinsinCentralTarim,NWChina.In:Bullen,T.D.andWang,Y.C.(eds.),Water-RockInteraction,Taylor&FrancisGroup,London.p.703-707.蔡春芳,2007.油气藏中热化学和微生物硫酸盐还原作用。矿物岩石地球化学通报,26卷(增),pp.260-262。蔡春芳、邬光辉、李开开、陈利新、李梅、李宏涛,2007.塔中地区古生界热化学硫酸盐还原作用与原油中硫的成因。矿物岩石地球化学通报26(1),44-48.Cai,C.F.,Li,H.T.,Qin,MK.,Luo,XR.,Wang,F.Y.,Ou,G.X.,2007.Biogenicandpetroleum-relatedore-formingprocessesinDongshenguraniumdeposit,NWChina.OreGeologyReviews32,262-274.【PDF】Cai,C.F.,Dong,H.L.,Li,H.T.,Xiao,X.K.,Ou,G.X.,Zhang,C.M.,2007.MineralogicalandgeochemicalevidenceforcoupledbacterialuraniummineralizationandhydrocarbonoxidationintheShashagetaideposit,NWChina.ChemicalGeology236,167-179.【PDF】Wei,ZB,J.Moldowan,JM,Fago,F.,Dahl,J.E.,Cai,C.F.andPeters,K.E.,2007.OriginsofThiadiamondoidsandDiamondoidthiolsinPetroleum.ASAPEnergyFuels,21(6):3431-3436.Zhang,CM,Zhao,H.,Hu,M.,Xiao,Q.,Li,J.,Cai,C.F.,2007.AsimplecorrelationfortheviscosityofheavyoilsfromLiaoheBasin,NEChina.Source.JournalofCanadianPetroleumTechnology46(4),8-11.Li,HT,Cai,CF,He,H.,Li,K.K..,2007.MicrobialuraniummineralizationandhydrocarbonoxidationintheQianjiadiandeposit,NEChina.GeochimicaCosmochimiActa71,A570-A570.Li,HT,Cai,CF,Li,KK,Luo,X.R.,2007.Biogenicsphericalmagnetiteandcoffinitefromsandstone-typeuraniumdepositinDongshengarea.In:Bullen,T.D.andWang,Y.C.(eds.),Water-RockInteraction,Taylor&FrancisGroup,London.p.881-885.李开开、蔡春芳、李宏涛,2007.塔中奥陶系稀土元素与87Sr/86Sr分布及其意义。矿物岩石地球化学通报,26卷(增),pp.296-298。李宏涛、蔡春芳、李开开、罗晓容,2007.东胜砂岩型铀矿床低温微生物成矿模式探讨.矿物岩石地球化学通报,26卷(增),pp.292-293。李宏涛、蔡春芳、李开开、罗晓容,2007.内蒙古东胜铀矿床球状磁铁矿的成因及意义.地质论评,53(4),564-570.李宏涛、蔡春芳、罗晓容、李开开,2007.鄂尔多斯北部直罗组中烃类包裹体地球化学特征及来源分析.沉积学报25(3)467-473.李宏涛、蔡春芳、罗晓容、孙希勇,2007.内蒙古东胜地区中侏罗统砂岩沉积物源的地球化学证据.地质科学,42(2),353-361.2006年Worden,R.H.,Cai,C.F.,2006.Discussion:GeochemicalcharacteristicsoftheZhaolanzhuangsourgasaccumulationandthermochemicalsulfatereductionintheJixianSagofBohaiBayBasinbyZhangetal.(OrganicGeochemistry36,1717-1730).OrganicGeochemistry37,511-514.Cai,C.F.,Peng,L.C.,Mei,B.W.,Xiao,Y.K.,2006.B,Sr,OandHisotopiccompositionsofformationwatersfromtheBachuBulge,TarimBasin.ActaGeologicalSinica80(4):550-556.2005年蔡春芳、李宏涛.2005.沉积盆地热化学硫酸盐还原作用评述.地球科学进展,20(5),14-19.Cai,C.F.,Hu,GY,He,H.,Li,J,Li,JF,Wu,Y.S.,2005.GeochemicalcharacteristicsandoriginofnaturalgasandthermochemicalsulfatereductioninOrdoviciancarbonatesintheOrdosBasin,China.JournalofPetroleumScienceandEngineering48(3/4),209-226.Cai,C.F.,Worden,R.H.,Wolff,G.A.,Bottrell,S.H.,Wang,D.L.,Li,X.,2005.OriginofsulfurrichoilsandH2SinTertiarylacustrinesectionsoftheJinxianSag,BohaiBayBasin,China.AppliedGeochemistry20,1427-1444.2004年Cai,C.F.,He,H.,Mei,B.W.,Xiao,Y.K.,2004,OriginofbrinesfromtheBachuUplift,TarimBasin,China:chemistryandd11Bevidence.In:WantyRBandSealRR(Eds.),Water-RockInteraction2004.London:TaylorandFrancisGroup,pp.367-372Cai,C.F.,Xie,Z.Y.,Worden,R.H.,Hu,G.Y.,Wang,L.S.,He,H.,2004,Methane-dominatedthermochemicalsulphatereductionintheTriassicFeixianguanFormationEastSichuanBasin,China:towardspredictionoffatalH2Sconc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