赵新福
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资料介绍
个人简历
男,1982年生,江苏镇江人。2004年6月毕业于中国地质大学(武汉)资源勘查工程基地班,获学士学位;2006年6月获得中国地质大学(武汉)矿物学、岩石学、矿床学硕士学位,2010年1月获得香港大学矿床学博士学位。2010-2013年在香港大学从事博士后研究工作。2013年4月回母校中国地质大学(武汉)资源学院工作,2018年获得国家自然科学基金优秀青年基金资助。主要从事热液矿床的成矿作用机理研究,主要研究方向为岩浆热液铁-铜-金-稀土矿床。主持和参与了多项国家自然科学基金和科技部重点研发项目,发表SCI论文50余篇,包括第一作者或通讯作者在EconomicGeology,MineraliumDeposita,GeochimicaetCosmochimicaActa,ChemicalGeology和AmericanMineralogist等矿床学和矿床地球化学的重要期刊上发表论文约20篇,论文SCI引用超2000次。二、教学情况本科生课程:《矿床地球化学》、《矿床学》研究生课程:《高级矿床学》、《矿床学理论与矿产勘查前沿》、《区域成矿学》四、近期主要研究项目[1]蚀变矿物和流体包裹体卤族元素LA-ICPMS原位分析对热液矿床成因的指示:以长江中下游成矿带为例(国家自然科学基金面上项目,编号41972074,2020-2023),主持[2]矿床学(国家自然科学基金优秀青年项目,编号41822203,2019-2021),主持[3]华北克拉通破坏成矿响应的集成研究(国家自然科学重大研究计划集成项目,编号91514303,2016-2017),主持[4]康滇铁铜成矿带典型矿床成矿机制:矿物微区地球化学和年代学制约(国家自然科学面上项目,编号91514303,2014-2018),主持[5]华北东部巨量金来源、迁移与富集机理(国家重点研发计划深地资源勘查开采专项,编号2016YFC0600104,2016-2020),参加[6]稀有金属元素成矿的构造-岩浆深部过程(科技部深地资源探测专项项目,编号2017YFC0602401,2017-2021),参加[7]矽卡岩型富铁矿形成机制及控制因素(国家重点基础研究发展计划(973计划)课题,编号2012CB416802:2012-2016),参加研究领域
1、岩浆热液铁-铜-金-稀土成矿系统:包括铁氧化物-铜-金(IOCG)矿床、玢岩铁矿(IOA)、矽卡岩型矿床和碳酸岩相关的稀土矿床等2、盆地流体铜-铅-锌-铀成矿系统3、成因矿物学反演热液成矿系统形成和演化过程及其找矿指示4、华南前寒武纪构造演化与成矿作用近期论文
28)Zhao,X.-F.,Chen,W.-T.,Li,X.-C.,Zhou,M.-F.,2020.IronOxideCopper-GoldDepositsinChina:AReviewandPerspectivesonOreGenesis.In:Goldfarb,R.,Chang,Z.(Eds.),MineralDepositsofChina.SEGSpecialPublication.Volume22,inpress27)Xiong,L.,Zhao,X.*,Wei,J.,Jin,X.,Fu,L.,Lin,Z.,2020.LinkingMesozoiclodegolddepositstometal-fertilizedlowercontinentalcrustintheNorthChinaCraton:EvidencefromPbisotopesystematics.ChemicalGeology:119440.26)Su,Z.-K.,Zhao,X.-F.*,Zeng,L.-P.,Zhao,K.-D.,Hofstra,A.H.,2019.Tourmalineboronandstrontiumisotopesystematicsrevealmagmaticfluidpulsesandexternalfluidinfluxinagiantironoxide-apatite(IOA)deposit.GeochimicaetCosmochimicaActa,259:233-252.25)Zeng,L.-P.,Zhao,X.-F.*,Hammerli,J.,Fan,T.-W.-T.,Spandler,C.,2019.Trackingfluidsourcesforskarnformationusingscapolitegeochemistry:anexamplefromtheJinshandianironskarndeposit,EasternChina.MineraliumDeposita.DOI:10.1007/s00126-019-00914-324)Su,J.-H.,Zhao,X.-F.*,Li,X.-C.,Hu,W.,Chen,M.,Xiong,Y.-L.,2019.GeologicalandgeochemicalcharacteristicsoftheMiaoyasyenite-carbonatitecomplex,CentralChina:ImplicationsfortheoriginofREE-Nb-enrichedcarbonatite.OreGeologyReviews,113:103101.23)赵新福*,李占轲*,赵少瑞,毕诗健,李建威,2019.华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统.地球科学,44(1):52-68.22)李建威,赵新福,邓晓东,谭俊,胡浩,张东阳,李占轲,李欢,荣辉,杨梅珍,曹康,靳晓野,隋吉祥,俎波,昌佳,吴亚飞,文广,赵少瑞2019.新中国成立以来中国矿床学研究若干重要进展.中国科学:地球科学,49:1720-1771.21)林祖苇,赵新福*,熊乐,朱照先,2019.胶东三山岛金矿床黄铁矿原位微区微量元素特征及对矿床成因的指示.地球科学进展,34(4):399-413.20)陈伟,赵新福,李晓春,周美夫,2019.中国铁氧化物-铜-金(IOCG)矿床的基本特征及研究进展.岩石学报,35(1):99-118.19)纪敏,赵新福*,曾丽平,范田纬腾,2018.鄂东南铜绿山矿床石榴子石显微结构及微区成分对成矿过程的指示.岩石学报,34(9):2716-2732.18)Zhao,X.-F.*,Zhou,M.-F.,Su,Z.-K.,Li,X.-C.,Chen,W.T.,Li,J.-W.,2017.Geology,geochronology,andgeochemistryoftheDahongshanFe-Cu-(Au-Ag)deposit,SWChina:ImplicationsfortheformationofIOCGdepositsinintracratonicriftsettings.EconomicGeology,112(3):603-628.17)Bi,S.-J.,Zhao,X.-F.*,2017.40Ar/39ArdatingoftheJiehegolddepositintheJiaodongPeninsula,easternNorthChinaCraton:Implicationsforregionalgoldmetallogeny.OreGeologyReviews,86:639-651.16)Zeng,L.-P.,Zhao,X.-F.*,Li,X.-C.,Hu,H.,McFarlane,C.,2016.InsituelementalandisotopicanalysisoffluorapatitefromtheTaocunmagnetite-apatitedeposit,EasternChina:Constraintsonfluidmetasomatism.AmericanMineralogist,101(11):2468-2483.15)Su,Z.-K.,Zhao,X.-F.*,Li,X.-C.,Zhou,M.-F.,2016.UsingelementalandboronisotopiccompositionsoftourmalinetotracefluidevolutionsofIOCGsystems:TheworldclassDahongshanFe-CudepositinSWChina.ChemicalGeology,441:265-279.14)Zhao,X.-F.*,Zhou,M.-F.,Gao,J.-F.,Li,X.-C.,Li,J.-W.,2015.InsituSrisotopeanalysisofapatitebyLA-MC-ICPMS:constraintsontheevolutionoforefluidsoftheYinachangFe-Cu-REEdeposit,SouthwestChina.MineraliumDeposita,50(7):871-884.13)Li,X.,Zhao,X.,Zhou,M.-F.,Chen,W.T.,Chu,Z.,2015.FluidinclusionandisotopicconstraintsontheoriginofthePaleoproterozoicYinachangFe-Cu-(REE)deposit,southwestChina.EconomicGeology,110(5):1339-1369.12)Zhou,M.-F.,Zhao,X.-F.,Chen,W.T.,Li,X.-C.,Wang,W.,Yan,D.-P.,Qiu,H.-N.,2014.ProterozoicFe-CumetallogenyandsupercontinentalcyclesofthesouthwesternYangtzeBlock,southernChinaandnorthernVietnam.Earth-ScienceReviews,139(0):59-82.11)Zhao,X.-F.,Zhou,M.-F.,Li,J.-W.,SelbyD.,LiC.,LiX.-H.andQi,L.,2013.SulfideRe–OsandRb–SrisotopicagesandthetectonicenvironmentoftheKangdianFe–Cumetallogenicprovince,SWChina.EconomicGeology,108(6):1489-1498.10)Zhao,X.-F.,Zhou,M.-F.,Li,J.-W.,andQi,L.,2013.LatePaleoproterozoicsediment-hostedstratiformcopperdepositsinSouthChina:Theirpossiblelinktothesupercontinentcycle.MineraliumDeposita,48(1):129-136.9)Huang,X.-W.,Zhao,X.-F.*,Qi,L.,Zhou,M.-F.,2013.Re-OsandSisotopicconstraintsontheoriginsoftwomineralizationeventsattheTangdansedimentaryrock-hostedstratiformCudeposit,SWChina.ChemicalGeology,347(0):9-19.8)Zhao,X.-F.,Zhou,M.-F.,Hitzman,M.W.,Li,J.-W.,Bennett,M.,Meighan,C.andAnderson,E.,2012.LatePaleoproterozoictoEarlyMesoproterozoicTangdanSedimentaryRock-HostedStrata-boundCopperDeposit,YunnanProvince,SouthwestChina.EconomicGeology,107:357-375.7)Zhao,X.-F.andZhou,M.-F.,2011.Fe–CudepositsintheKangdianregion,SWChina:AProterozoicIOCG(iron-oxide–copper–gold)metallogenicprovince.MineraliumDeposita46:731-747.6)Zhao,X.-F.,Zhou,M.-F.,Li,J.-W.,Sun,M.,Gao,J.-F.,Sun,W.-H.,Yang,J.-H.,2010.LatePaleoproterozoictoearlyMesoproterozoicDongchuanGroupinYunnan,SWChina:ImplicationsfortectonicevolutionoftheYangtzeBlock.PrecambrianResearch,182:57-69.5)Li,J.-W.,Zhao,X.-F.,Zhou,M.-F.,Ma,C.-Q.,deSouza,Z.andVasconcelos,P.,2009.LateMesozoicmagmatismfromtheDayeregion,easternChina:U–Pbages,petrogenesis,andgeodynamicimplications.ContributionstoMineralogyandPetrology,157:383-409.4)Li,J.-W.,Zhao,X.-F.,Zhou,M.-F.,Vasconcelos,P.,Ma,C.-Q.,Deng,X.-D.,deSouza,Z.S.,Zhao,Y.-X.,Wu,G.,2008.OriginoftheTongshankouporphyry–skarnCu–Modeposit,easternYangtzecraton,EasternChina:geochronological,geochemical,andSr–Nd–Hfisotopicconstraints.MineraliumDeposita,43(3):315-336.3)Zhao,X.-F.,Zhou,M.-F.,Li,J.-W.,andWu,F.-Y.,2008.AssociationofNeoproterozoicA-andI-typegranitesinSouthChina:ImplicationsforgenerationofA-typegranitesinasubduction-relatedenvironment.ChemicalGeology,257:1-15.2)赵新福,李建威,马昌前,郎银生,2007.北淮阳古碑花岗闪长岩侵位时代及地球化学特征:对大别山中生代构造体制转换的启示.岩石学报,23(6):1392-1402.1)赵新福,李建威,马昌前,2006.鄂东南铁铜矿集区铜山口铜(钼)矿床40Ar/39Ar年代学及对区域成矿作用的指示.地质学报,80(6):849-862.标签: 资源学院 中国地质大学(武汉)
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