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1、Xiang,H.,Zhang,L.,*Zhong,Z.,Santosh,M.,Zhou,H.,Zhang,H.,Zheng,J.,andZheng,S.,Ultrahigh-temperaturemetamorphismandanticlockwiseP–T–tpathofPaleozoicgranulitesfromnorthQinling-Tongbaiorogen,CentralChina,GondwanaResearch,2012,21(2-3):559-576;
2、Zhang,L.,Zhong,X.,Zhang,H.,Sun,W.,andXiang,X.,Theformationoffoliated(garnet-bearing)granitesintheTongbai-Dabieorogenicbelt:partialmeltingofsubductedcontinentalcrustduringexhumation.JournalofmetamorphicGeology,2009,27:789–803;
3、向华,张利*,钟增球,张宏飞,郑建平,刘理.北桐柏地区镁铁质麻粒岩锆石U-Pb年代学及变质作用.岩石学报,2009,25(2):348-358;
4、Zhang,L.,Zhong,Z.,Wang,L.,Zhang,B.,PbisotopemappinginTongbai-Dabieorogenicbelt,CentralChina.ActaGeologicaSinica,2008,82(1):126-133;
5、曾雯,张利*,周汉文,钟增球,向华,刘锐,靳松,吕新前,李春忠.华夏地块古元古代基底的加里东期再造:锆石U-Pb年龄、Hf同位素和微量元素制约.科学通报,2008,53(3):225-344;
6、向华,张利*,钟增球,曾雯,刘锐,靳松.浙西南变质基底基性-超基性变质岩锆石U-Pb年龄、Hf同位素研究:华夏地块变质基底对华南印支期造山的响应.中国科学,2008,38(4):401-413;
7、刘锐,张利*,周汉文,钟增球,曾雯,向华,靳松,吕新前李春忠.闽西北加里东期混合岩及花岗岩的成因:同变形地壳深熔作用.岩石学报,2008,24(6):1205-1222;
8、靳松,张利*,钟增球,周汉文,向华,曾雯,刘锐.浙闽地区新元古代变火山岩系岩石地球化学特征及其地质意义.矿物岩石,2008,28(1):97-105;
9、靳松,张利*,钟增球,周汉文,向华,曾雯,刘锐,吕新前,李春忠.浙闽地区华夏地块新元古代变沉积岩地球化学特征及其地质意义.地球科学,2008,33(6):764-774;
10、Zhang,L.,Zhong,Z.,Zhang,H.,Sun,W.,Santosh,M.,andXiang,H.,ThehighpressuremetamorphicunitintheTongbai-Dabieorogenicbelt,China:Geochemistry,Sr-Ndisotopesandimplicationsonpetrogenesis.ChemicalGeology,2013,inreview;
11、Zhang,L.,Fang,J.,andJoeckel,R.,MicrobialBiomassandCommunityStructureinAlkalineLakesoftheNebraskaSandHills,USA.OrganicGeochemistry,2013,inreview;
12、张利,何卫红.在野外教学实习中实践素质教育-周口店野外实践教学的体会.中国地质大学学报(社会科学版),2008,增刊(5月):31-34;
13、向华,张利*,钟增球,周汉文,曾雯.榍石:U-Pb定年及变质P-T-t轨迹的建立.地球科学进展,2007,22(12):50-59;
14、张利,钟增球,张宏飞,王林森.桐柏-大别造山带高压变质单元岩石Pb同位素组成.地球科学,2005,30(6):729-737;
15、张利,钟增球,张宏飞,王林森.从Pb同位素组成看东秦岭官坡超高压变质岩片的走势.矿物岩石,2005,25(2):60-63;
16、Zhang,L.,Zhong,Z.,Zhang,B.,Liu,Y.,andHu,S.,GeochemistryandPetrogenesisofFoliatedGarnet-bearingGranitesinHighPressureMetamorphicUnitoftheTongbai-DabieOrgogenicBelt.InFengChanggened.,TheproceedingsoftheChinaAssociationforScienceandTechnology,Beijing:SciencePressUSAInc,2005,2(2):409-419;
17、张利,钟增球,张本仁,刘勇胜,胡圣虹.桐柏-大别造山带高压变质单元面理化(含榴)花岗岩地球化学及其岩石成因的限制.地球化学,2004,33(3):232-242;
18、Zhang,L.,Zhang,H.,Zhong,Z.,Zhang,B.,andWang,L.,GeochemicalcharacteristicsofPbisotopeofthehigh-pressuremetamorphicrocksandfoliatedgranitesfromtheHPunitofTongbai-Dabieorogenicbelt.EarthScience-JournalofChinaUniversityofGeosciences,2003,14(4):310-318;
19、Zhang,H.,Zhang,L.,Harris,N.,Jin,L.,andYuan,H.,U-Pbzirconages,geochemicalandisotopiccompositionsofgranitoidsinSongpan-Garzefoldbelt,easternTibetanPlateau:Constraintsonpetrogenesisandtectonicevolutionofthebasement,ContributionstoMineralogyandPetrology,2006,152(1):75-88;
20、Liu,R.,Zhou,H.,Zhang,L.,Zhong,Z.,Zeng,W.,Xiang,H.,Jin,S.,Lu,X.,andLi,C.,ZirconU-PbagesandHfisotopecompositionsoftheMayuanmigmatitecomplex,NWFujianProvince,SoutheastChina:constraintsonthetimingandnatureofaregionaltectonothermaleventassociatedwiththeCaledonianorogeny,Lithos,2010,119:163-180;
21、Zhang,H.,Parrish,R.,Zhang,L.,Xu,W.,Yuan,H.,Shan,G.,andCrowley,Q.,ReplytothecommentbyZhangetal.on:"FirstfindingofA-typeandadakiticmagmatismassociationinSongpan-Garzefoldbelt,easternTibetanPlateau:Implicationforlithoshpericdelamination".Lithos,2008,103(3-4):565-568;
22、Zhang,H.,Parrish,R.,Zhang,L.,Xu,W.,Yuan,H.,Shan,G.,andCrowley,Q.,A-typegraniteandadakiticmagmatismassociationinSongpan-Garzefoldbelt,easternTibetanPlateau:Implicationforlithosphericdelamination.Lithos,2007,97(3-4):323-335;
23、张宏飞,肖龙,张利,袁洪林,靳兰兰.扬子陆块西北缘碧口块体印支期花岗岩类地球化学和Pb-Sr-Nd同位素组成:限制岩石成因及其动力学背景.中国科学D辑,2007,37(4):460-470;
24、张宏飞,靳兰兰,张利,NigelHarris,周炼,胡圣虹,张本仁.西秦岭花岗岩类地球化学和Pb-Sr-Nd同位素组成对基底性质及其构造属性的限制.2007,中国科学D辑,35(10):914-926;
25、刘锐,周汉文,张利,钟增球,曾雯,向华,靳松,吕新前李春忠.华夏地块古元古代陆壳再造:锆石微量元素与U-Pb和Lu-Hf同位素证据.科学通报,2009,54(7):906-917;
26、Fang,J.,Zhang,L.,andBazylinski,D.A,.Thedeep-seapiezosphereandpiezophiles:geomicrobiologyandbiogeochemistry.TrendsinMicrobiology,2010,18:413-422;
27、Fang,J.,andZhang,L.,2011.Genomics,metagenomicsandmicrobialoceanography–aseaofopportunities.ScienceinChina(EarthSciences),54(4):473-480;
28、方家松、张利.探索深部生物圈.中国科学,2011,41(6):750-759;
29、Suo,S.,Zhong,Z.,Zhang,L.,Zhou,H.,andYou,Z.,TwoDiscreteUHPandHPMetamorphicBeltsintheCentralOrogenicBelt,China.JournalofChinaUniversityofGeosriences,2006,17(3):189–200;
30、Wang,J.,Li,J.,Dasgupta,S.,Zhang,L.,andFang,J.,AlterationsinmembranelipidcompositionofpiezophilicGram-positivebacteriumSporosarcinasp.DSK25athighpressures.ComparativeBiochemistryandPhysiology,2013,accepted;
31、Fang,J.,Li,C.,Zhang,L.,Kato,C.,andBartlett,D.G.,Hydrogenisotoperatiosoffattyacidsasevidencefortheco-existingandindependentlyoperatingdualbiosyntheticpathwaysinpiezophilicbacteri.JournaloftheAmericanChemicalSociety,2013,inreview;
32、张宏飞,靳兰兰,张利,袁洪林,周炼,张本仁.基底岩系和花岗岩类Pb-Nd同位素组成限制祁连山带的构造属性.地球科学,2006,31(1):57-65;
33、何卫红,张利.地质类大学生科研活动存在的问题及建议.中国地质大学学报(社会科学版),2008,增刊(5月):123-126;
34、王林森,张利.用双稀释法测定地质样品中的铅同位素组成.矿物岩石,2003,23(2):44-48;
35、王林森,张利,贾望鲁.大别-苏鲁超高压榴辉岩中Pb同位素分析的实验技术研究.地球科学,2003,28(2):137-142;
36、Zhang,H.,Harris,N.,Parrish,R.,Kelley,S.,Zhang,L.,Rogers,N.,Argels,T.,King,J.,Causesandconsequencesofprotractedmeltingofthemid-crustexposedintheNorthHimalayanantiform.EarthandPlanetaryScienceletters,2004,228:195-212;
37、Richards,A.,Parrish,R.,Harris,N.,ArglesT.,andZhang,L.,CorrelationoflithotectonicunitsacrosstheeasternHimalaya,Bhutan.Geology,2006,5:341-344;
38、Zhang,H.,Gao,S.,Zhong,Z.,Zhang,B.,Zhang,L.,Hu,S.,GeochemicalandSr-Nd-PbisotopiccompositionsofCretaceousgranitoids:constraintsontectonicframeworkandcrustalstructureoftheDabieshanultrahigh-pressuremetamorphicbelt,China.ChemicalGeology,2002,186(3-4):281-299;
39、Dasgupta,S.,Fang,J.,Brake,S.S.,Hasiotis,S.T.,Zhang,L.,BiosynthesisofsterolsandwaxestersbyEuglenaofacidminedrainagebiofilms:ImplicationsforeukaryoticevolutionandtheearlyEarth.ChemicalGeology,2012,306–307:139–145;
40、Dasgupta,S.,Fang,J.,Brake,S.S.,Hasiotis,S.T.,Zhang,L.,StableCarbonIsotopicCompositionofLipidsinEuglena-DominatedBiofilmsfromanAcidMineDrainageSite:ImplicationsofCarbonLimitation,MicrobialPhysiology,andBiosyntheticPathways.ChemicalGeology,2013,accepted;
41、Zhang,H.,Zhong,Z.,Gao,S.,Zhang,B.,Zhang,L.,Hu,S.,Hou,Q.,PbandNdisotopiccompositionoftheJigongshangranite:constraintsoncrustalstructureofTongbaishaninthemiddlepartoftheQinling–Tongbai–Dabieorogenicbelt,CentralChina.Lithos,2004,73(3-4):215-227;
42、Zhang,H.,Zhang,B.,Harris,H.,Zhang,L.,Chen,Y.,Chen,N.,Zhao,Z.,U–PbzirconSHRIMPages,geochemicalandSr–Nd–PbisotopiccompositionsofintrusiverocksfromtheLongshan–TianshuiareainthesoutheastcorneroftheQilianorogenicbelt,China:Constraintsonpetrogenesisandtectonicaffinity,JournalofAsianEarthSciences,2006,27(6):751-764;
43、Suo,S.,Zhong,Z.,Zhou,H.,You,Z.,Zhang,H.,Zhang,L.,TectonicevolutionoftheDabei-SuluUHPandHPmetamorphicbelts,East-CentralChina:structuralrecordinUHProcks.InternationalGeologyReview,2005,47:1207-1221;
44、张宏飞,N.Harris,R.Parrish,张利,赵志丹.北喜马拉雅萨迦穹窿中苦堆和萨迦淡色花岗岩的U-Pb年龄及其地质意义.科学通报,2004,49(20):2090-2094;
45、侯青叶,赵志丹,张本仁,张宏飞,张利,陈岳龙.青藏高压东北缘特提斯构造域界线的探讨.岩石学报,2006,22(3):567-577;
46、侯青叶,赵志丹,张宏飞,张本仁,张利,陈岳龙.西秦岭-松潘构造结古洋地幔地球化学特征及构造归属探讨.岩石学报,2006,22(12):2901-2909;
47、索书田,钟增球,周汉文,张利,游振东.大别—苏鲁区超高压(UHP)变质岩的多阶段构造折返过程.地球科学—中国地质大学学报,2012,37(1):1-17;
48、张小文,向华,钟增球,周汉文,张利,杨念,王婧.海南尖峰岭岩体热液锆石U-Pb定年及微量元素研究:对热液作用及抱伦金矿成矿时代的限定.地球科学-中国地质大学学报,2009,34(6):921-930;
49、张宏飞,NigelHarris,RandallParrish,张利,赵志丹,李德威.北喜马拉雅淡色花岗岩地球化学:区域对比、岩石成因及其构造意义.地球科学-中国地质大学学报,2005,30(3):275-288;(EI)
50、周炼,高山,刘勇胜,凌文黎,张利.扬子克拉通北缘碎屑沉积岩地球化学特征及意义.地球科学,2007,32(1):29-38;
51、周炼,陈孝红,李志宏,刘勇胜,张利.三峡地区寒武纪三叠纪古海水变化特征:来自牙形石的证据.地球科学,2006,31(1):136-142;
52、李晔,周汉文,钟增球,向华,曾雯,祁冬梅,张利.北秦岭早古生代两期变质作用:来自松树沟基性岩岩石学及锆石U-Pb年代学的记录.地球科学—中国地质大学学报,2012,37(增刊):111-124;
53.ShamikDasgupta,方家松,李江涛,张利,王嘉妮,韦兵兵.现代酸性矿山废水环境中的真核微生物:生物多样性、生理学、生物地球化学特征及其对古环境和早期生命演化的指示.第四纪研究,2013,33(1):68-78;
54、钟增球,索书田,张利,周汉文,游振东.岩石塑性流变学-大别-苏鲁高压超高压变质带的构造学.中国地质大学出版社,2007.9;
55、Fang,J.,andZhang,L.,Piezophilicbacteria.In:TheEncyclopediaofGeobiology,theSpringerEncyclopediaofEarthSciencesSeries(J.ReitnerandV.Thiel,eds.),Springer-VerlagHeidelbergGermany,2011
56、Zhang,L.,Zhong,Z.,Zhang,H.,Sun,W.,Xiang,H.,Fang,J.,Geochemistryandpetrogenesisoffoliated(garnet-bearing)granitesintheTongbai-Dabieorogenicbelt.GeochimicaEtCosmochimicaActa(20thAnnualW.M.Goldschmidtconferenceabstracts),2010,74:A1209-1209;
57、Zhang,L.,Zhong,Z.,Xiang,H.,ZhangH.,andZheng,J.,MetamorphismofmaficgranuliteofnorthTongbai,centralChina:evidencefromzirconU-Pbdating.2009AGUFallMeeting,SanFrancisco,California,USA:V51B-1677;
58、Zhang,L.,Zhong,Z.,Xiang,H.,Zhang,H.,ZhengJ.,andLiu,L.,StudiesonP-T-tofmaficgranulitesfromnorthTongbai,centralChina.GeochimicaEtCosmochimicaActa(19thAnnualW.M.Goldschmidtconferenceabstracts),2009,73(13):A1507-1507;
59、Zhang,L.,Zhong,Z.,Zhou,H.,Zeng,W.,Xiang,H.,Liu,R.,andJin,S.,ZirconU-Pbdating,HfisotopesandtraceelementscharacteristicsofthemigmatitesinTianjingpingarea,northwesternFujianProvince.GeochimicaEtCosmochimicaActa(18thAnnualW.M.Goldschmidtconferenceabstracts),2008,72(12):A1086-1086;
60、Zhang,L.,andZhong,Z.,PartialmeltingduringtheexhumationoftheUHProcksinDabieshanMassif.GeochimicaEtCosmochimicaActa(17thAnnualW.M.Goldschmidtconferenceabstracts),2007,71(15):A1158-1158;
61、Zhang,L.,andZhong,Z.,GeochemicalandisotopicconstraintsongenesisoffoliatedgranitesinHPunitoftheTongbai-Dabieorogenicbelt.GeochimicaEtCosmochimicaActa(16thAnnualW.M.Goldschmidtconferenceabstracts),2006,70(18):A735-735;
62、Zhang,L.,Zhang,H.,andZhong,Z.,GeochemicalstructureofPbisotopesinTongbai-Dabiearea.EarthandPlanetaryScienceletters(15thGoldschmidtconferenceabstracts),2005:A655-655;
63、Dasgupta,S.,Fang,J.,Zhang,L.,Kato,C.,Li,J.,andBartlett,D.H.,2012.CarbonandHydrogenIsotopeFractionationinLipidBiosynthesisofPiezophilicBacteria–ImplicationsforStudyingMicrobialMetabolismandCarbonCycleinDeepBiosphere.2012AGUFallMeetingabstract;
64、Zhang,H.,Harris,N.,Parrish,R.,andZhang,L.,AssociationofgraniticmagmatismintheSongpan-Garzefoldbelt,easternTibetPlateau:Implicationforlithosphericdelamination,GeochimicaEtCosmochimicaActa(16thAnnualW.M.Goldschmidtconferenceabstracts),2006,S5-09.