郯庐断裂带晚第三纪以来的浅部挤压活动与深部过程
|
摘要
郯庐断裂带晚第三纪以来持续遭受着挤压 ,使前期大规模的断陷盆地抬升、消亡 ,近代还是中国东部最大的地震活动带。断裂带所遭受的近WE向的挤压 ,是西太平洋弧后扩张和印度板块向北碰撞中的构造挤出作用产生的区域动力。断裂带在新生代挤压活动中切入上地幔 ,出现了地幔剪切、地幔交代、部分熔融等深部过程 ,最终形成了挤压背景下的陆内断裂带大规模的玄武岩喷发
Thrusting time of the Tan Lu fault zone has been a controversial issue for long. Recently, many lines of evidence has proved that wide spread compression initiated on the fault zone between Eogene and Neogene, which has given rise to the uplift and consumption of many previous large faulted basins. Since Neogene period the fault zone has continued to suffer from compression, which resulted in many times of thrusting on the fault. The fault zone is currently the largest seismically active belt in eastern China. The compressive activities on the fault zone were dominated by thrusting with small amount of right lateral displacement sometimes and were often associated with the development of NW striking left lateral wrench faults. Margins of basins on the fault zone were intensely involved in the thrusting which caused the formation of shuttered zone and folds. Measurements of paleostress and present stress fields show that the fault zone has suffered nearly E W compression since Neogene due to the back arc spreading of the west Pacific Ocean and tectonic extrusion produced by the northward collision of the Indian Plate. Basalt eruption extensively occurred along the fault zone in Cenozoic, indicating that the fault zone cuts deeply into the upper mantle. Lithological character of the Cenozoic basalts demonstrates that the cutting depth of the fault increased from Paleogene to Quaternary gradually. Geoscience transects reveal obvious intensification of asthenoshperic upwelling beneath the Tan Lu fault zone, which demonstrates that the fault zone cut through the entire lithosphere. Deformed mantle derived xenoliths, such as mylonitic peridotite xenolith, in the basalts reflect that mantle shearing appeared in mantle involved by the fault. Metasomatic minerals in the xenoliths as well as geochemical features of the basalts and xenoliths all suggest that the involved mantle experienced extensive metasomatism. The mantle shearing and metasomatism are related closely and help each other. They also help partial melting in the involved mantle. Under these backgrounds, large scale partial melting appeared in the upper mantle involved by the fault zone. At last, large scale basalt eruption took place along the intracontinental fault zone under the compressive setting. Therefore, integrate active processes of the fault zone since Neogene consist of the thrusting, basin inversion and basalt eruption near the surface as well as the upper mantle shearing, metasomatism and partial melting at deeps.
Thrusting time of the Tan Lu fault zone has been a controversial issue for long. Recently, many lines of evidence has proved that wide spread compression initiated on the fault zone between Eogene and Neogene, which has given rise to the uplift and consumption of many previous large faulted basins. Since Neogene period the fault zone has continued to suffer from compression, which resulted in many times of thrusting on the fault. The fault zone is currently the largest seismically active belt in eastern China. The compressive activities on the fault zone were dominated by thrusting with small amount of right lateral displacement sometimes and were often associated with the development of NW striking left lateral wrench faults. Margins of basins on the fault zone were intensely involved in the thrusting which caused the formation of shuttered zone and folds. Measurements of paleostress and present stress fields show that the fault zone has suffered nearly E W compression since Neogene due to the back arc spreading of the west Pacific Ocean and tectonic extrusion produced by the northward collision of the Indian Plate. Basalt eruption extensively occurred along the fault zone in Cenozoic, indicating that the fault zone cuts deeply into the upper mantle. Lithological character of the Cenozoic basalts demonstrates that the cutting depth of the fault increased from Paleogene to Quaternary gradually. Geoscience transects reveal obvious intensification of asthenoshperic upwelling beneath the Tan Lu fault zone, which demonstrates that the fault zone cut through the entire lithosphere. Deformed mantle derived xenoliths, such as mylonitic peridotite xenolith, in the basalts reflect that mantle shearing appeared in mantle involved by the fault. Metasomatic minerals in the xenoliths as well as geochemical features of the basalts and xenoliths all suggest that the involved mantle experienced extensive metasomatism. The mantle shearing and metasomatism are related closely and help each other. They also help partial melting in the involved mantle. Under these backgrounds, large scale partial melting appeared in the upper mantle involved by the fault zone. At last, large scale basalt eruption took place along the intracontinental fault zone under the compressive setting. Therefore, integrate active processes of the fault zone since Neogene consist of the thrusting, basin inversion and basalt eruption near the surface as well as the upper mantle shearing, metasomatism and partial melting at deeps.
引文
李开善,1987,郯庐断裂带构造应力场初步探讨,中国地质科学院562综合大队集刊第6号。
陈道公.1992.郯庐断裂带中南段新生代玄武岩地球化学〔A〕.见:刘若新主编.中国新生代火山岩年代学与地球化学.北京:地震出版社.171～200.
CHENDao gong.1992.ThegeochemistryofCenozoicbasaltsatthemiddle southernsegmentofTanLufaultzone〔A〕.In:LIURuo xin,ed.TheAgesandGeochemistryofCenozoicVolcanicRocksinChina.Beijing:Seismo logicalPress.171～200(inChinese).
陈道公,彭子成.1986.山东临朐玄武岩的Nd、Sr、Pb同位素体系〔J〕.科学通报,1:45～48.
CHENDao gong,PENGZi cheng.1986.Nd,Sr,PbisotopicsystemofbasaltsinLinquregion,ShandongProvince〔J〕.ChineseScienceBulletin,(1):45～48(inChinese).
陈道公,杨杰东,王银喜.1990苏皖鲁某些新生代火山岩的钕同位素组成及意义〔J〕.科学通报,12:925～927.
CHENDao gong,YANGJie dong,WANGYin xi.1990.NdisotopiccomponentsandsignificanceofsomeCenozoicvolcanicrocksfromJiangsu,AnhuiandShandongProvinces,China〔J〕.ChineseScienceBulletin,(12):925～927(inChinese).
陈沪生,张永鸿,徐师文,等.1999.下扬子及邻区岩石圈结构构造特征与油气资源评价〔M〕.北京:地质出版社.
CHENHu sheng,ZHANGYong hong,XUShi wen,etal.1999.LithosphericStructuresandEvaluationofHydro carbonResourcesinLowerYangtzeandAdjacentRegions〔M〕.Beijing:GeologicalPublishingHouse(inChi nese).
陈全茂,李忠飞.1998.辽河盆地东部凹陷构造及含油气性分析〔M〕.北京:地质出版社.141～148.
CHENQuan mao,LIZhong fei.1998.DepressionStructuresinEastLiaoheBasinandPetroliferousAnalysis〔M〕.Beijing:GeologicalPublishingHouse.141～148(inChinese).
陈希祥.1985.郯庐断裂(中段)挽近时期的新活动〔J〕.海洋地质与第四纪地质,5(1):91～97.
CHENXi xiang.1985.RecentactivityoftheTanLufaultzone(middlepart)〔J〕.MarineGeologyandQuaternaryGeology,5(1):91～97(inChinese).
陈义贤.1985.辽河裂谷盆地断裂演化序次和油气藏形成模式〔J〕.石油学报,6(2):1～11.
CHENYi xian.1985.TheevolutionoffaultsandformationofoilandgasreservoirsintheLiaoheriftvalley〔J〕.Ac taPetroleiSinica,6(2):1～11(inChinese).
鄂莫岚,赵大升.1987.中国东部新生代玄武岩及深源岩石包体〔M〕.北京:科学出版社.
EMo lan,ZHAODa sheng,eds.1987.CenozoicBasaltsandDeep derivedXenolithsinEastChina〔M〕.Beijing:SciencePress(inChinese).
方仲景,丁梦麟,向宏发,等.1986.郯庐断裂带的基本特征〔J〕.科学通报,(1):52～55.
FANGZhong jing,DINGMeng lin,XIANGHong fa,etal.1986.BasiccharacteristicsoftheTanLuFaultzone〔J〕.ChineseScienceBulletin,(1):52～55(inChinese).
高维明,李家灵,孙竹友.1984.沂沭活动断裂及其地震构造〔A〕.构造地质论丛(三).北京:地质出版社.263～271.
GAOWei ming,LIJia ling,SUNZhu you.1984.Yishuactivefaultanditsseismicstructure〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.263～271(inChinese).
国家地震局地质研究所.1987.郯庐断裂〔M〕.北京:地震出版社.
InstituteofGeology,StateSeismologicalBureau.1987.TheTanLuFaultZone〔M〕.Beijing:SeismologicalPress(inChinese).
国家地震局中国地震区划图编委会.1991.中国及邻区地震震源机制图及说明书〔Z〕.北京:地震出版社.
StateSeismologicalBureau.1991.MapofFocalMechanismsofChinaanditsAdjacentAreas〔Z〕.Beijing:Seismolo gicalPress(inChinese).
林传勇,何永年,史兰斌.1990.糜棱岩型幔源包体及其地质意义〔A〕.国际大陆岩石圈构造演化与动力学讨论会论文集.北京:科学出版社.165～172.
LINChuan yong,HEYong nian,SHILan bin.1990.Mylonitetypemantle derivedxenolithsandtheirgeologicalsignificances〔A〕.ProceedingsofInternationalContinentalLithosphereEvolutionandDynamics.Beijing:Sci encePress.165～172(inChinese).
林传勇,徐义刚,张小鸥,等.1996.中国东部上地幔岩石变形特征、流体的作用及软流层(体)的初步探讨〔A〕.见:杜乐天等主编.地幔流体与软流层(体)地球化学.北京:地质出版社.312～340.
LINChuan yong,XUYi gang,ZHANGXiao ou,etal.1996.Deformationofmantlerocks(EastChina),fluidsandasthenosphere〔A〕.In:DULe tianetal.,eds.GeochemistryofMantleFluidsandAsthenosphere.Bei jing:GeologicalPublishingHouse.312～340(inChinese).
刘茂强,杨丙中,邓俊国,等.1993.伊通舒兰地堑地质构造特征及其演化〔M〕.北京:地质出版社.
LIUMao qiang,YANGBing zhong,DENGJun guo,etal.1993.GeologicalTectonicFeaturesandEvolutionofYitongShulanGraben〔M〕.Beijing:GeologicalPublishingHouse(inChinese).
刘若新主编.1992.中国新生代火山岩年代学与地球化学〔C〕.北京:地震出版社.LIURuo xin,ed.1992.TheAgeandGeochemistryofCenozoicVolcanicRocksinChina〔C〕.Beijing:Seismologi calPress(inChinese).
卢华复,俞鸿年,丁幼文,等.1984.试论郯庐断裂带中段新构造期构造应力场的演化〔A〕.构造地质论丛(三).北京:地质出版社.107～115.
LUHua fu,YUHong nian,DINGYou wen,etal.1984.OntheevolutionofthestructuralstressfieldsintheareaofthemiddlesegmentoftheTanchengLujiangfracturezoneinneotectonicperiod〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.107～115(inChinese).
陆克政,漆家福,戴俊生,等.1997.渤海湾新生代含油气盆地构造模式〔M〕.北京:地质出版社.LUKe zheng,QIJia fu,DAIJun sheng,etal.1997.TectonicModelsofCenozoicPetroliferousBasininBohaiBay〔M〕.Beijing:GeologicalPublishingHouse(inChinese).
卢造勋,夏怀宽.1992.内蒙古东乌珠穆沁旗至辽宁东海地学断面〔Z〕.北京:地震出版社.
LUZao xun,XIAHuai kuan.1992.GeoscienceTransectfromDongUjimjinQi,InnerMongoliatoDonggou,Liaoning〔Z〕.Beijing:SeismologicalPress(inChinese).
马杏垣,刘昌铨,刘国栋.1991.江苏响水至内蒙古满都拉地学断面〔Z〕.北京:地质出版社.
MAXing yuan,LIUChang quan,LIUGuo dong.1991.GeoscienceTransectfromXiangshui,JiangsutoMandal,InnerMongolia〔Z〕.Beijing:GeologicalPublishingHouse(inChinese)
牛漫兰,朱光,宋传中,等.2000.郯庐断裂带火山活动与深部地质过程新认识〔J〕.地质科技情报,19(3):21～26.
NIUMan lan,ZHUGuang,SONGChuan zhong,etal.2000.VolcanicactivitiesanddeepgeologicalprocessesintheTanLufaultzone〔J〕.GeologicalScienceandTechnologyInformation,19(3):21～26(inChinese).
强祖基,胡思颐,胡海燕,等.1984.郯庐断裂带的构造与演化特征〔A〕.构造地质论丛(三).北京:地质出版社.107～115.
QIANGZu ji,HUSi yi,HUHai yan,etal.1984.TectonicsandevolutionoftheTanchengLujiangdeepfaultzone〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.107～115(inChinese).
强祖基,叶士忠.1985.1668年山东莒县-郯城8级大震区的活动断裂特征〔J〕.地震地质,7(2):19～26.
QANGZu ji,YEShi zhong.1985.TheCharacteristicsoftheactivefaultsinthe1668greatearthquakearea,Juxi anTancheng,ShandongProvince〔J〕.SeismologyandGeology,7(2):19～26(inChinese).
任有保,于有兰.1996.沂水北部沂沭断裂带构造透镜体特征〔J〕.山东地质,12(1):76～83.
RENYou bao,YUYou lan.1996.CharacteristicsoftectoniclensesinthenorthernYishuiareaoftheYishuiFaultzone〔J〕.GeologyofShandong,12(1):76～83(inChinese).
商玉强,文琼英,张宝政.1992.沂沭断裂带内部王氏组的沉积环境及构造意义〔J〕.山东地质,8(1):30～41.
SHANGYu qiang,WENQiong ying,ZHANGBao zheng.1992.DepositionalenvironmentoftheWangsiForma tionintheYishuFaultzoneanditstectonicimplication〔J〕.GeologyofShandong,8(1):30～41(inChinese).
孙武城,徐杰,杨主恩,等.1992.上海奉贤至内蒙古阿拉善左旗地学断面〔Z〕.北京:地震出版社.
SUNWu cheng,XUJie,YANGZhu en,etal.1992.GeoscienceTransectfromFengxian,ShanghaitoAlxaZuo qi,InnerMongolia〔Z〕.Beijing:SeismologicalPress(inChinese).
汤有标,姚大全.1990.郯庐断裂带赤山段晚更新世以来的活动性〔J〕.中国地震,6(2):63～69.
TANGYou biao,YAODa quan.1990.PostlatePleistoceneactivityofChishansegmentoftheTanLuFaultzone〔J〕.EarthquakeResearchinChina,6(2):63～69(inChinese).
汤有标,姚大全.1990.郯庐断裂带南段新活动性的初步研究〔J〕.地震研究,13(2):155～165.
TANGYou biao,YaoDa quan.1990.PreliminarystudiesonnewactivityofthesouthernpartoftheTanLuFaultzone〔J〕.JournalofSeismologicalResearch,13(2):155～165(inChinese).
万天丰.1992.山东省构造演化与应力场〔J〕.山东地质,8(2):70～101
.WANTian feng.1992.TectonicevolutionandstressfieldsinShandongProvince〔J〕.GeologyofShandong,8(2):70～101(inChinese).
王小凤,李中坚,陈柏林,等.2000.郯庐断裂带〔M〕.北京:地质出版社.320～321.
WANGXiao feng,LIZhong jian,CHENBo lin,etal.2000.TheTanLuFaultZone〔M〕.Beijing:GeologicalPublishingHouse.320～321(inChinese).
徐嘉炜.1978.试论郯庐断裂带的平移及其地质找矿意义〔J〕.地质矿产研究,(5):1～30.
XUJia wei.1978.OndisplacementoftheTanLufaultzoneanditsgeologicalandmineralprospectingsignificance〔J〕.ResearchofGeologyandMinerals,(5):1～30(inChinese).
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾〔J〕.地质论评,38(4):316～324.
XUJia wei,MAGuo feng.1992.Ten yearsreviewonresearchontheTanLufaultzone〔J〕.GeologicalReview,38(4):316～324(inChinese).
徐义刚,MenziesMA ,林传勇.1997.吉林伊通幔源包体的微量元素组成及其成因岩石学意义〔J〕.岩石学报,13(1):14～25
XUYi gang,MenziesMA ,LINChuan yong,etal.1997.Traceelementcompositionsofmantle derivedxenolithsfromYitong,JilinProvinceandtheirpetrogeneticimplication〔J〕.ActaPetrologicaSinica,13(1):14～25(inChinese).
张宝政,刘玉海.1982.佳木斯伊通断裂带的基本特征及其与郯庐断裂带的关系〔J〕.长春地质学院学报,(1):29～39.
ZHANGBao zheng,LIUYu hai.1982.BasiccharacteristicsoftheJaimusiYitongFaultzoneanditsrelationtotheTanLuFaultzone〔J〕.JournalofChangchunUniversityofEarthSciences,(1):29～39(inChinese).
周进高,赵宗举,邓红婴.1999.合肥盆地构造演化及含油气性分析〔J〕.地质学报,73(1):15～24.
ZHOUJin gao,ZHAOZong ju,DENGHong ying.1999.StructuralevolutionoftheHefeiBasinandpetroliferousanalysis〔J〕.ActaGeologicaSinica,73(1):15～24(inChinese).
夏林圻,夏祖春,徐学义.1996.地幔橄榄岩捕虏体中的流体包裹体、岩浆包裹体和玻璃〔A〕.见:杜乐天等主编.地幔流体与软流层(体)地球化学.北京:地质出版社.230～271.
XIALin qi,XIAZu chun,XUXue yi.1996.Thefluidinclusions,magmaticinclusionsandglassesinmantleperi dotite〔A〕.In:DULe tianetal.,eds.GeochemistryofMantleFluidsandAsthenosphere.Beijing:GeologicalPublishingHouse.230～271(inChinese).
许浚远.1997.依舒地堑新生代构造演化〔J〕.地球科学,22(4):406～410.
XUJun yuan.1997.CenozoicstructuralevolutionoftheYiSuGraben〔J〕.EarthSciences,22(4):406～410(inChinese).
严俊尹,马前贵.1992.渤海海城的郯庐扭断裂及含油气盆地的发育〔J〕.地球科学,17(1):31～37
YANJun yin,MAQian gui.1992.TheTanchengLujiangwrenchfaultsysteminBohaiBayarea〔J〕.EarthSci ence,17(1):31～37(inChinese).
张小鸥.1995.伊通地堑上地幔剪切带〔J〕.地震地质,17(2):167～176.
ZHANGXiao ou.1995.TheuppermantleshearzoneofYitongGraben〔J〕.SeismologyandGeology,17(2):167～176(inChinese).
朱光,刘国生,王道轩,等.2000.郯庐断裂带的脉动式伸展活动〔J〕.高校地质学报,6(3):396～404.
ZHUGuang,LIUGuo sheng,WANGDao xuan,etal.2000.PulsativeextensionalactivitiesoftheTanLuFaultzone〔J〕.GeologicalJournalofChinaUniversities,6(3):396～404(inChinese).
朱光,徐嘉炜.1998.郯庐断裂带的平移幅度、平移时代及其构造模式〔A〕.见:陈毓川等主编.第30届国际地质大会论文集,第14卷(构造地质学、地质力学).北京:地质出版社.167～175.
ZHUGuang,XUJia wei.1998.Displacement,timingandtectonicmodeloftheTanLuFaultzone〔A〕.Proceed ingsof30thInternationalGeologicalCongress,Vol.14.Beijing:GeologicalPublishingHouse.167～175(inChinese).
DownesH .1990.Shearzonesintheuppermantle—relationbetweengeochemicalenrichmentanddeformationinmantleperidotite〔J〕.Geology,18:374～377.
FreyFA ,HansonLA .1971.Rareearthabundanceinsomeultramaficrocks〔J〕.JGeophysRes,76:2057～2072.XuJW ,ZhuG .1994.TectonicmodelsoftheTanLuFaultzone,easternChina〔J〕.InternationalGeologyRe view,36:771～784.
陈道公.1992.郯庐断裂带中南段新生代玄武岩地球化学〔A〕.见:刘若新主编.中国新生代火山岩年代学与地球化学.北京:地震出版社.171～200.
CHENDao gong.1992.ThegeochemistryofCenozoicbasaltsatthemiddle southernsegmentofTanLufaultzone〔A〕.In:LIURuo xin,ed.TheAgesandGeochemistryofCenozoicVolcanicRocksinChina.Beijing:Seismo logicalPress.171～200(inChinese).
陈道公,彭子成.1986.山东临朐玄武岩的Nd、Sr、Pb同位素体系〔J〕.科学通报,1:45～48.
CHENDao gong,PENGZi cheng.1986.Nd,Sr,PbisotopicsystemofbasaltsinLinquregion,ShandongProvince〔J〕.ChineseScienceBulletin,(1):45～48(inChinese).
陈道公,杨杰东,王银喜.1990苏皖鲁某些新生代火山岩的钕同位素组成及意义〔J〕.科学通报,12:925～927.
CHENDao gong,YANGJie dong,WANGYin xi.1990.NdisotopiccomponentsandsignificanceofsomeCenozoicvolcanicrocksfromJiangsu,AnhuiandShandongProvinces,China〔J〕.ChineseScienceBulletin,(12):925～927(inChinese).
陈沪生,张永鸿,徐师文,等.1999.下扬子及邻区岩石圈结构构造特征与油气资源评价〔M〕.北京:地质出版社.
CHENHu sheng,ZHANGYong hong,XUShi wen,etal.1999.LithosphericStructuresandEvaluationofHydro carbonResourcesinLowerYangtzeandAdjacentRegions〔M〕.Beijing:GeologicalPublishingHouse(inChi nese).
陈全茂,李忠飞.1998.辽河盆地东部凹陷构造及含油气性分析〔M〕.北京:地质出版社.141～148.
CHENQuan mao,LIZhong fei.1998.DepressionStructuresinEastLiaoheBasinandPetroliferousAnalysis〔M〕.Beijing:GeologicalPublishingHouse.141～148(inChinese).
陈希祥.1985.郯庐断裂(中段)挽近时期的新活动〔J〕.海洋地质与第四纪地质,5(1):91～97.
CHENXi xiang.1985.RecentactivityoftheTanLufaultzone(middlepart)〔J〕.MarineGeologyandQuaternaryGeology,5(1):91～97(inChinese).
陈义贤.1985.辽河裂谷盆地断裂演化序次和油气藏形成模式〔J〕.石油学报,6(2):1～11.
CHENYi xian.1985.TheevolutionoffaultsandformationofoilandgasreservoirsintheLiaoheriftvalley〔J〕.Ac taPetroleiSinica,6(2):1～11(inChinese).
鄂莫岚,赵大升.1987.中国东部新生代玄武岩及深源岩石包体〔M〕.北京:科学出版社.
EMo lan,ZHAODa sheng,eds.1987.CenozoicBasaltsandDeep derivedXenolithsinEastChina〔M〕.Beijing:SciencePress(inChinese).
方仲景,丁梦麟,向宏发,等.1986.郯庐断裂带的基本特征〔J〕.科学通报,(1):52～55.
FANGZhong jing,DINGMeng lin,XIANGHong fa,etal.1986.BasiccharacteristicsoftheTanLuFaultzone〔J〕.ChineseScienceBulletin,(1):52～55(inChinese).
高维明,李家灵,孙竹友.1984.沂沭活动断裂及其地震构造〔A〕.构造地质论丛(三).北京:地质出版社.263～271.
GAOWei ming,LIJia ling,SUNZhu you.1984.Yishuactivefaultanditsseismicstructure〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.263～271(inChinese).
国家地震局地质研究所.1987.郯庐断裂〔M〕.北京:地震出版社.
InstituteofGeology,StateSeismologicalBureau.1987.TheTanLuFaultZone〔M〕.Beijing:SeismologicalPress(inChinese).
国家地震局中国地震区划图编委会.1991.中国及邻区地震震源机制图及说明书〔Z〕.北京:地震出版社.
StateSeismologicalBureau.1991.MapofFocalMechanismsofChinaanditsAdjacentAreas〔Z〕.Beijing:Seismolo gicalPress(inChinese).
林传勇,何永年,史兰斌.1990.糜棱岩型幔源包体及其地质意义〔A〕.国际大陆岩石圈构造演化与动力学讨论会论文集.北京:科学出版社.165～172.
LINChuan yong,HEYong nian,SHILan bin.1990.Mylonitetypemantle derivedxenolithsandtheirgeologicalsignificances〔A〕.ProceedingsofInternationalContinentalLithosphereEvolutionandDynamics.Beijing:Sci encePress.165～172(inChinese).
林传勇,徐义刚,张小鸥,等.1996.中国东部上地幔岩石变形特征、流体的作用及软流层(体)的初步探讨〔A〕.见:杜乐天等主编.地幔流体与软流层(体)地球化学.北京:地质出版社.312～340.
LINChuan yong,XUYi gang,ZHANGXiao ou,etal.1996.Deformationofmantlerocks(EastChina),fluidsandasthenosphere〔A〕.In:DULe tianetal.,eds.GeochemistryofMantleFluidsandAsthenosphere.Bei jing:GeologicalPublishingHouse.312～340(inChinese).
刘茂强,杨丙中,邓俊国,等.1993.伊通舒兰地堑地质构造特征及其演化〔M〕.北京:地质出版社.
LIUMao qiang,YANGBing zhong,DENGJun guo,etal.1993.GeologicalTectonicFeaturesandEvolutionofYitongShulanGraben〔M〕.Beijing:GeologicalPublishingHouse(inChinese).
刘若新主编.1992.中国新生代火山岩年代学与地球化学〔C〕.北京:地震出版社.LIURuo xin,ed.1992.TheAgeandGeochemistryofCenozoicVolcanicRocksinChina〔C〕.Beijing:Seismologi calPress(inChinese).
卢华复,俞鸿年,丁幼文,等.1984.试论郯庐断裂带中段新构造期构造应力场的演化〔A〕.构造地质论丛(三).北京:地质出版社.107～115.
LUHua fu,YUHong nian,DINGYou wen,etal.1984.OntheevolutionofthestructuralstressfieldsintheareaofthemiddlesegmentoftheTanchengLujiangfracturezoneinneotectonicperiod〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.107～115(inChinese).
陆克政,漆家福,戴俊生,等.1997.渤海湾新生代含油气盆地构造模式〔M〕.北京:地质出版社.LUKe zheng,QIJia fu,DAIJun sheng,etal.1997.TectonicModelsofCenozoicPetroliferousBasininBohaiBay〔M〕.Beijing:GeologicalPublishingHouse(inChinese).
卢造勋,夏怀宽.1992.内蒙古东乌珠穆沁旗至辽宁东海地学断面〔Z〕.北京:地震出版社.
LUZao xun,XIAHuai kuan.1992.GeoscienceTransectfromDongUjimjinQi,InnerMongoliatoDonggou,Liaoning〔Z〕.Beijing:SeismologicalPress(inChinese).
马杏垣,刘昌铨,刘国栋.1991.江苏响水至内蒙古满都拉地学断面〔Z〕.北京:地质出版社.
MAXing yuan,LIUChang quan,LIUGuo dong.1991.GeoscienceTransectfromXiangshui,JiangsutoMandal,InnerMongolia〔Z〕.Beijing:GeologicalPublishingHouse(inChinese)
牛漫兰,朱光,宋传中,等.2000.郯庐断裂带火山活动与深部地质过程新认识〔J〕.地质科技情报,19(3):21～26.
NIUMan lan,ZHUGuang,SONGChuan zhong,etal.2000.VolcanicactivitiesanddeepgeologicalprocessesintheTanLufaultzone〔J〕.GeologicalScienceandTechnologyInformation,19(3):21～26(inChinese).
强祖基,胡思颐,胡海燕,等.1984.郯庐断裂带的构造与演化特征〔A〕.构造地质论丛(三).北京:地质出版社.107～115.
QIANGZu ji,HUSi yi,HUHai yan,etal.1984.TectonicsandevolutionoftheTanchengLujiangdeepfaultzone〔A〕.CollectionofStructuralGeology(3).Beijing:GeologicalPublishingHouse.107～115(inChinese).
强祖基,叶士忠.1985.1668年山东莒县-郯城8级大震区的活动断裂特征〔J〕.地震地质,7(2):19～26.
QANGZu ji,YEShi zhong.1985.TheCharacteristicsoftheactivefaultsinthe1668greatearthquakearea,Juxi anTancheng,ShandongProvince〔J〕.SeismologyandGeology,7(2):19～26(inChinese).
任有保,于有兰.1996.沂水北部沂沭断裂带构造透镜体特征〔J〕.山东地质,12(1):76～83.
RENYou bao,YUYou lan.1996.CharacteristicsoftectoniclensesinthenorthernYishuiareaoftheYishuiFaultzone〔J〕.GeologyofShandong,12(1):76～83(inChinese).
商玉强,文琼英,张宝政.1992.沂沭断裂带内部王氏组的沉积环境及构造意义〔J〕.山东地质,8(1):30～41.
SHANGYu qiang,WENQiong ying,ZHANGBao zheng.1992.DepositionalenvironmentoftheWangsiForma tionintheYishuFaultzoneanditstectonicimplication〔J〕.GeologyofShandong,8(1):30～41(inChinese).
孙武城,徐杰,杨主恩,等.1992.上海奉贤至内蒙古阿拉善左旗地学断面〔Z〕.北京:地震出版社.
SUNWu cheng,XUJie,YANGZhu en,etal.1992.GeoscienceTransectfromFengxian,ShanghaitoAlxaZuo qi,InnerMongolia〔Z〕.Beijing:SeismologicalPress(inChinese).
汤有标,姚大全.1990.郯庐断裂带赤山段晚更新世以来的活动性〔J〕.中国地震,6(2):63～69.
TANGYou biao,YAODa quan.1990.PostlatePleistoceneactivityofChishansegmentoftheTanLuFaultzone〔J〕.EarthquakeResearchinChina,6(2):63～69(inChinese).
汤有标,姚大全.1990.郯庐断裂带南段新活动性的初步研究〔J〕.地震研究,13(2):155～165.
TANGYou biao,YaoDa quan.1990.PreliminarystudiesonnewactivityofthesouthernpartoftheTanLuFaultzone〔J〕.JournalofSeismologicalResearch,13(2):155～165(inChinese).
万天丰.1992.山东省构造演化与应力场〔J〕.山东地质,8(2):70～101
.WANTian feng.1992.TectonicevolutionandstressfieldsinShandongProvince〔J〕.GeologyofShandong,8(2):70～101(inChinese).
王小凤,李中坚,陈柏林,等.2000.郯庐断裂带〔M〕.北京:地质出版社.320～321.
WANGXiao feng,LIZhong jian,CHENBo lin,etal.2000.TheTanLuFaultZone〔M〕.Beijing:GeologicalPublishingHouse.320～321(inChinese).
徐嘉炜.1978.试论郯庐断裂带的平移及其地质找矿意义〔J〕.地质矿产研究,(5):1～30.
XUJia wei.1978.OndisplacementoftheTanLufaultzoneanditsgeologicalandmineralprospectingsignificance〔J〕.ResearchofGeologyandMinerals,(5):1～30(inChinese).
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾〔J〕.地质论评,38(4):316～324.
XUJia wei,MAGuo feng.1992.Ten yearsreviewonresearchontheTanLufaultzone〔J〕.GeologicalReview,38(4):316～324(inChinese).
徐义刚,MenziesMA ,林传勇.1997.吉林伊通幔源包体的微量元素组成及其成因岩石学意义〔J〕.岩石学报,13(1):14～25
XUYi gang,MenziesMA ,LINChuan yong,etal.1997.Traceelementcompositionsofmantle derivedxenolithsfromYitong,JilinProvinceandtheirpetrogeneticimplication〔J〕.ActaPetrologicaSinica,13(1):14～25(inChinese).
张宝政,刘玉海.1982.佳木斯伊通断裂带的基本特征及其与郯庐断裂带的关系〔J〕.长春地质学院学报,(1):29～39.
ZHANGBao zheng,LIUYu hai.1982.BasiccharacteristicsoftheJaimusiYitongFaultzoneanditsrelationtotheTanLuFaultzone〔J〕.JournalofChangchunUniversityofEarthSciences,(1):29～39(inChinese).
周进高,赵宗举,邓红婴.1999.合肥盆地构造演化及含油气性分析〔J〕.地质学报,73(1):15～24.
ZHOUJin gao,ZHAOZong ju,DENGHong ying.1999.StructuralevolutionoftheHefeiBasinandpetroliferousanalysis〔J〕.ActaGeologicaSinica,73(1):15～24(inChinese).
夏林圻,夏祖春,徐学义.1996.地幔橄榄岩捕虏体中的流体包裹体、岩浆包裹体和玻璃〔A〕.见:杜乐天等主编.地幔流体与软流层(体)地球化学.北京:地质出版社.230～271.
XIALin qi,XIAZu chun,XUXue yi.1996.Thefluidinclusions,magmaticinclusionsandglassesinmantleperi dotite〔A〕.In:DULe tianetal.,eds.GeochemistryofMantleFluidsandAsthenosphere.Beijing:GeologicalPublishingHouse.230～271(inChinese).
许浚远.1997.依舒地堑新生代构造演化〔J〕.地球科学,22(4):406～410.
XUJun yuan.1997.CenozoicstructuralevolutionoftheYiSuGraben〔J〕.EarthSciences,22(4):406～410(inChinese).
严俊尹,马前贵.1992.渤海海城的郯庐扭断裂及含油气盆地的发育〔J〕.地球科学,17(1):31～37
YANJun yin,MAQian gui.1992.TheTanchengLujiangwrenchfaultsysteminBohaiBayarea〔J〕.EarthSci ence,17(1):31～37(inChinese).
张小鸥.1995.伊通地堑上地幔剪切带〔J〕.地震地质,17(2):167～176.
ZHANGXiao ou.1995.TheuppermantleshearzoneofYitongGraben〔J〕.SeismologyandGeology,17(2):167～176(inChinese).
朱光,刘国生,王道轩,等.2000.郯庐断裂带的脉动式伸展活动〔J〕.高校地质学报,6(3):396～404.
ZHUGuang,LIUGuo sheng,WANGDao xuan,etal.2000.PulsativeextensionalactivitiesoftheTanLuFaultzone〔J〕.GeologicalJournalofChinaUniversities,6(3):396～404(inChinese).
朱光,徐嘉炜.1998.郯庐断裂带的平移幅度、平移时代及其构造模式〔A〕.见:陈毓川等主编.第30届国际地质大会论文集,第14卷(构造地质学、地质力学).北京:地质出版社.167～175.
ZHUGuang,XUJia wei.1998.Displacement,timingandtectonicmodeloftheTanLuFaultzone〔A〕.Proceed ingsof30thInternationalGeologicalCongress,Vol.14.Beijing:GeologicalPublishingHouse.167～175(inChinese).
DownesH .1990.Shearzonesintheuppermantle—relationbetweengeochemicalenrichmentanddeformationinmantleperidotite〔J〕.Geology,18:374～377.
FreyFA ,HansonLA .1971.Rareearthabundanceinsomeultramaficrocks〔J〕.JGeophysRes,76:2057～2072.XuJW ,ZhuG .1994.TectonicmodelsoftheTanLuFaultzone,easternChina〔J〕.InternationalGeologyRe view,36:771～784.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心