华东地区现代地壳应力场及地震断层错动性质
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摘要
使用143组中、小地震单震震源机制解和17组小区域综合机制解资料,统计分析了华东地区的现代构造应力场特征。华东地区现今处在NEE向(80°左右)主压、NNW向(350°左右)主张应力场的控制下;主应力作用方式以水平和近水平为主。在应力场方向和作用方式基本一致的背景上,不同地震构造分区存在一些差异,这些差异可能与相应区域主要活动断裂的主体分布方向有关,可能表征了现存构造对地震错动特征的影响和控制作用。现代中、小地震震源机制解,历史中、强地震和现代有感地震最内等震线长轴方向等资料显示华东地区地震主要沿NE,NW2个方向破裂错动,兼有NNE,NEE,NWW或近EW方向。以走滑和近走滑方式为主,兼有少量斜向滑动。地震断层的错动方式存在某些分区差异。华东地区历史中、强地震以NE向破裂错动为主,而现代中强地震在陆域以NW-SE为主,海域NE,NW兼有。
Statistic analysis has been made on the characteristics of the contemporary tectonic stress field of East China based on 143 sets of single focal mechanical solutions of moderate and small earthquakes and on 17 sets of composite focal mechanism solutions. Results show that the stress field of East China exhibits a NNE (about 80°) oriented principal compression and NNW (about 350°) principal tension, and the principal stresses are mainly horizontal or near-horizontal. In the context of basically consistent orientation and action mode of stress field, there are some variations in the stress field among different seismotectonic regions, which are possibly related to the distribution of major active faults in the respective regions. This indicates that fault slip may be dominated or affected by existing tectonics. The feature of earthquake fracture and the orientation of fault slip of contemporary earthquakes in East China have been analyzed with data of focal mechanism solutions of contemporary moderate and small events, and of the orientations of major axis for innermost isoseismal of historical and contemporary events and so on. It indicates that the earthquake fractures of East China extend at large in NE and NW directions, and sometimes with NNE, NEE, NWW, or near EW directions. The movements of earthquake faults are mainly of strike-slip or near strike-slip with oblique-slip component. There exist some regional variations in the movement of earthquake faults. The historical moderate and strong events in East China exhibit mainly a NE trending slip, while the modern events show the NW-SE trending slip on the land and NE and NW trend slip in the sea area.
Statistic analysis has been made on the characteristics of the contemporary tectonic stress field of East China based on 143 sets of single focal mechanical solutions of moderate and small earthquakes and on 17 sets of composite focal mechanism solutions. Results show that the stress field of East China exhibits a NNE (about 80°) oriented principal compression and NNW (about 350°) principal tension, and the principal stresses are mainly horizontal or near-horizontal. In the context of basically consistent orientation and action mode of stress field, there are some variations in the stress field among different seismotectonic regions, which are possibly related to the distribution of major active faults in the respective regions. This indicates that fault slip may be dominated or affected by existing tectonics. The feature of earthquake fracture and the orientation of fault slip of contemporary earthquakes in East China have been analyzed with data of focal mechanism solutions of contemporary moderate and small events, and of the orientations of major axis for innermost isoseismal of historical and contemporary events and so on. It indicates that the earthquake fractures of East China extend at large in NE and NW directions, and sometimes with NNE, NEE, NWW, or near EW directions. The movements of earthquake faults are mainly of strike-slip or near strike-slip with oblique-slip component. There exist some regional variations in the movement of earthquake faults. The historical moderate and strong events in East China exhibit mainly a NE trending slip, while the modern events show the NW-SE trending slip on the land and NE and NW trend slip in the sea area.
引文
①蒋海昆等，2003，华东地区地震学短期预测方法研究，国家“十五”科技攻关计划子专题(2001 BA60 B01-04一01)研究报告。
①同第277页①
晁洪太,王锜,李家灵,等.1997.《山东省地震构造图》、《山东省新构造图》说明书[Z].济南:山东省地图出版社.CHAOHong tai,WANGQi,LIJia ling,etal.1997.Demonstrationof“SeismotectonicMapofShandongProvince”and“NeotectonicsMapofShandongProvince”[Z].CartographicPublishingHouseofShandongProvince,Jinan,China(inChinese).
陈棋福,郑大林,李桂萍,等.2002a.中国震例(1992—1994)[M].北京:地震出版社.15—36.CHENQi fu,ZHENGDa lin,LIGui ping,etal.2002a.EarthquakeCasesinChina(1992—1994)[M].Seismological Press,Beijing.15—36(inChinese).
陈棋福,郑大林,李桂萍,等.2002b.中国震例(1995—1996)[M].北京:地震出版社.165—199.CHENQi fu,ZHENGDA lin,LIGui ping,etal.2002b.EarthquakeCasesinChina(1995—1996)[M].Seismological Press,Beijing.165—199(inChinese).
方仲景,丁梦林,计凤桔,等.1980.郯城-庐江断裂带地震活动的地质分析[J].地震地质,2(4):39—44.FANGZhong jing,DINGMeng lin,JIFeng ju,etal.1980.GeologicalanalysisoftheseismicityintheTancheng Lu jiangFaultzone,EastChina[J].SeismologyandGeology,2(4):39—44(inChinese).
方仲景,丁梦林,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.ThefundamentalfeatureoftheTancheng Lujian Faultzone[J〕.ScienceBulletin,(1):52—55(inChinese).
蒋溥,戴丽思,徐峰,等.1983.华北断块现代构造断裂的动力学问题的地震研究[J].地震地质,5(1):15—28.JIANGPu,DAILi si,XUFeng,etal.1983.SeismologicalstudyofdynamicproblemsofrecentfractureintheNorth Chinafaultblockregion[J].SeismologyandGeology,5(1):15—28(inChinese).
李钦祖.1980.华北地壳应力场的基本特征[J].地球物理学报,23(4):376—387.LIQin zu.1980.ThefundamentalfeatureofcrustalstressfieldinNorthChina[J].ActaGeophisicaSinica,23(4):376—387(inChinese).
六省(市)震源机制小组.1981.由震源机制解推断苏鲁皖豫地区现代构造应力场[J].地震地质,3(1):19—28.UnitedGroupofFocalMechanismStudy.1981.StudyofrecenttectonicstressfieldofJiangsu Sandong Anhui Henan regionfromfocalmechanismsolutions[J].SeismologyandGeology,3(1):19—28(inChinese).
马宏生,张国民,刘杰,等.2003.中国大陆及其邻区强震活动与活动地块关系研究[J].地学前缘,10(特刊):74—80.MAHong sheng,ZHANGGuo min,LIUJie,etal.2003.Correlationbetweenstrongearthquakeactivityandactive crustalblockinChinamainlandanditsadjacentregions[J].EarthScienceFrontiers,10(Suppl):74—80(in Chinese).
马淑田,张德存.1999.1996年11月9日长江口以东海域MS6.1级地震的震源机制初步研究[A].见:上海市地震局编.上海市的地震与应急:1996年长江口以东海域地震研究文集.北京:地震出版社.32—41.MAShu tian,ZHANGDe cun.1999.PreliminaryresearchonfocalmechanismoftheM6.1earthquakeoccurringinthe EastChinaSeaontheeastoftheYangtzeRiverestuaryonNov.9,1996[A].In:EarthquakeAdministrationof ShanghaiMunicipality(ed).EarthquakeEmergencyResponseofShanghai:theCollectedWorksofResearchon theM6.1EarthquakeintheEastChinaSeaontheEastoftheYangtzeRiverEstuaryonNov.9,1996.Seismo logicalPress,Beijing.32—41(inChinese).
马宗晋.1987.中国大陆的地震层和地震线[A].见:国家地震局地壳应力研究所编.地壳构造与地壳应力文集(一).北京:地震出版社.1—7.MAZong jin.1987.TheseismogeniclayersandlinesinChina smainland[A].In:InstituteofCrustalDynamics,SSB(ed).TheCollectedWorksofCrustalStructureandCrustalStress.SeismologicalPress,Beijing.1—7(in Chinese).
马杏垣主编.1989.中国岩石圈动力学地图集[Z].北京:中国地图出版社.36—44.MAXing yuan(ed).1989.AtlasofLithosphereDynamicsofChina[Z].ChinaCartographicPublishingHouse,Beijing.36—44(inChinese).
魏光兴,周翠英,赵兴兰.1982.华北地区中小地震应力场的优势方向[J].地球物理学报,25(4):333—343.WEIGuang xing,ZHOUCui ying,ZHAOXing lan.1982.TheDominantdirectionsofstressfieldfromminorearth quakesinNorth EasternChina[J].ChineseJournalofGeophysics,25(4):333—343(inChinese).
魏光兴,周翠英,侯海峰,等.1985.聊城-兰考断裂带及其邻区现代地壳应力场与地震活动[J].华北地震科学,3(2):19—29.WEIGuang xing,ZHOUCui ying,HOUHai feng,etal.1985.ModerncruststressfieldandseismicityinLiaocheng LankaoFaultzoneanditsadjacentareas[J].NorthChinaEarthquakeSciences,3(2):19—29(inChinese).
魏光兴,刁守中,周翠英.1993.郯庐带地震活动性研究[M].北京:地震出版社.WEIGuang xing,DIAOShou zhong,ZHOUCui ying.1993.ResearchonSeismicityoftheTanluFaultZone[M].Seis mologicalPress,Beijing(inChinese).
汪素云,许忠淮.1985.中国东部大陆地震构造应力场[J].地震学报,7(1):17—32.WANGSu yun,XUZhong huai.1985.SeismotectonicstressfieldinEastChina[J].ActaSeismologicaSinica,7(1):17—32(inChinese).
吴大铭,张裕明,方仲景,等.1981.论中国郯庐断裂带的活动[J].地震地质,3(4):15—24.WUDa ming,ZHANGYu ming,FANGZhong jing,etal.1981.OntheactivityoftheTancheng LujiangFaultzonein China[J].SeismologyandGeology,3(4):15—24(inChinese).
吴少武,张绍治,刘仲芳.1988.郯庐断裂带江苏段活动特征[J].中国地震,4(3):158—161.WUShao wu,ZHANGShao zhi,LIUZhong fang.1988.ActivitycharacteristicsandearthquakesofJiangsusegment oftheTanluFault[J].EarthquakeResearchinChina,4(3):158—161(inChinese).
许忠淮,汪素云,黄雨蕊,等.1989.由大量地震资料推断的我国大陆构造应力场[J].地球物理学报,32(6):637—647.XUZhong huai,WANGSu yun,HUANGYu rui,etal.1989.ThetectonicstressfieldoftheChinesecontinentdeduced fromagreatnumberofearthquakes[J].ChineseJournalofGeophysics,32(6):636—647(inChinese).
许忠淮,阎明,赵仲和.1983.由多个小震推断的华北地区构造应力场的方向[J].地震学报,5(3):268—279.XUZhong huai,YANMing,ZHAOZhong he.1983.EvaluationofthedirectionoftectonicstressinNorthChinafrom recordeddataofalargenumberofsmallearthquakes[J].ActaSeismologicaSinica,5(3):268—279(inChi nese).
夏瑞良.1985.安徽区域地震应力场的分布特征[J].地震地质,7(3):13—22.XIARui liang.1985.CharacteristicdistributionofregionalseismicstressfieldinAnhuiProvince[J].Seismologyand Geology,7(3):13—22(inChinese).
谢富仁,崔效锋,赵建涛.2004.中国大陆及邻区现代构造应力场分区[J].地球物理学报,47(4):654—662.XIEFu ren,CUIXiao feng,ZHAOJian tao,etal.2004.RegionaldivisionoftherecenttectonicstressfieldinChina andadjacentareas[J].ChineseJournalofGeophysics,47(4):654—662(inChinese).
谢富仁,崔效锋,赵建涛.2003.中国大陆现代构造应力场与强震活动的关系[A].见:谢富仁等编.中国大陆地壳应力环境研究.北京:地质出版社.69—74.XIEFu ren,CUIXiao feng,ZHAOJian tao,etal.2003.Therelationshipbetweenrecenttectonicstressfieldand strongearthquakesinChinesemainland[A].In:XIEFu ren,etal(ed).Researchoncrustalstressstatein Chinaandadjacentarea.GeologicalPublishingHouse,Beijing.69—74(inChinese).
徐杰,马宗晋,陈国光,等.2003.中国大陆东部新构造期北西向断裂带的初步探讨[J].地学前缘,10(特刊):193—198.XUJie,MAZong jin,CHENGuo guang,etal.2003.NWtrendingactivefaultzonesinEasternChinesecontinentin neotectonictime[J].EarthScienceFrontiers,10(Suppl):193—198(inChinese).
鄢家全,时振梁,汪素云,等.1979.中国及邻区现代构造应力场的区域特征[J].地震学报,1(1):9—24.YANJia quan,SHIZhen liang,WANGSu yun,etal.1979.SomefeaturesoftherecenttectonicstressfieldofChin andenvirons[J].ChineseJournalofGeophysics,1(1):9—24(inChinese).
张肇诚,罗兰格,李海华,等.1988.中国震例(1966—1975)[M].北京:地震出版社.144—154.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1988.EarthquakeCasesinChina(1966—1975)[M].Seismologi calPress,Beijing.144—154(inChinese).
张肇诚,罗兰格,李海华,等.1990a.中国震例(1976—1980)[M].北京:地震出版社.286—301,357—384.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1988.EarthquakeCasesinChina(1976—1980)[M].SeismologicalPress,Beijing.286—301,357—384(inChinese).
张肇诚,罗兰格,李海华,等.1990b.中国震例(1981—1985)[M].北京:地震出版社.190—223.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1990b.EarthquakeCasesinChina(1981—1985)[M].Seismo logicalPress,Beijing.190—233(inChinese).
张肇诚,郑大林,徐京华.1999a.中国震例(1986—1988)[M].北京:地震出版社.156—173.ZHANGZhao cheng,ZHENGDa lin,XUJing hua.1999.EarthquakeCasesinChina(1986—1988)[M].Seismologi calPress,Beijing.156—173(inChinese).
张肇诚,郑大林,徐京华.1999b.中国震例(1989—1991)[M].北京:地震出版社.176—202.ZHANGZhao cheng,ZHENDa lin,XUjing hua,etal.1990b.EarthquakeCasesinChina(1989—1991)[M].Seis mologicalPress,Beijing.176—202(inChinese).
赵景珍,朱晤.1981.河南林县4.7级地震[J].地震学刊,(1):71—75.ZHAOJing zhen,ZHUWu.1981.TheM4.7EarthquakeofLinxianinHenanProvince[J].Journalofseismology,(1):71—75(inChinese).
周翠英,魏光兴.1987.沂沭带的现代构造应力场与地震活动[J].华北地震科学,5(2):29—39.ZHOUCui ying,WEIGuang xing.1987.RecenttectonicstressfieldandseismicityintheYihe ShuheFaultbelt[J].NorthChinaEarthquakeSciences,5(2):29—39(inChinese).
周翠英,华爱军,蒋海昆,等.2003.以格点尝试法求取的山东地区现代中小地震震源机制解[J].东北地震研究,19(1):1—11.ZHOUCui ying,HUAAi jun,JIANGHai kun,etal.2003.Focalmechanismsolutionsobtainedbygridpointstest methodforcontemporarymoderateandsmallearthquakesinShandongarea[J].SeismologicalResearchofNorth eastChina,19(1):1—11(inChinese).
周翠英,周焕鹏,魏光兴,等.1992.应力场方向的微动态变化及其研究意义[A〕.见:马宗晋主编.大陆多震层研究:国际大陆多震层学术讨论会选集.北京:地震出版社.230—239.ZHOUCui ying,ZHOUHuan peng,WEIGuang xing,etal.1992.Micro variationofstressfieldanditsimplication inresearch[A].In:MAZong jin(ed).StudiesontheContinentalSeismogenicLayer:ProceedingsofWork shoponContinentalSeismogenicLayer.SeismologicalPress,Beijing.230—239(inChinese).
①同第277页①
晁洪太,王锜,李家灵,等.1997.《山东省地震构造图》、《山东省新构造图》说明书[Z].济南:山东省地图出版社.CHAOHong tai,WANGQi,LIJia ling,etal.1997.Demonstrationof“SeismotectonicMapofShandongProvince”and“NeotectonicsMapofShandongProvince”[Z].CartographicPublishingHouseofShandongProvince,Jinan,China(inChinese).
陈棋福,郑大林,李桂萍,等.2002a.中国震例(1992—1994)[M].北京:地震出版社.15—36.CHENQi fu,ZHENGDa lin,LIGui ping,etal.2002a.EarthquakeCasesinChina(1992—1994)[M].Seismological Press,Beijing.15—36(inChinese).
陈棋福,郑大林,李桂萍,等.2002b.中国震例(1995—1996)[M].北京:地震出版社.165—199.CHENQi fu,ZHENGDA lin,LIGui ping,etal.2002b.EarthquakeCasesinChina(1995—1996)[M].Seismological Press,Beijing.165—199(inChinese).
方仲景,丁梦林,计凤桔,等.1980.郯城-庐江断裂带地震活动的地质分析[J].地震地质,2(4):39—44.FANGZhong jing,DINGMeng lin,JIFeng ju,etal.1980.GeologicalanalysisoftheseismicityintheTancheng Lu jiangFaultzone,EastChina[J].SeismologyandGeology,2(4):39—44(inChinese).
方仲景,丁梦林,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.ThefundamentalfeatureoftheTancheng Lujian Faultzone[J〕.ScienceBulletin,(1):52—55(inChinese).
蒋溥,戴丽思,徐峰,等.1983.华北断块现代构造断裂的动力学问题的地震研究[J].地震地质,5(1):15—28.JIANGPu,DAILi si,XUFeng,etal.1983.SeismologicalstudyofdynamicproblemsofrecentfractureintheNorth Chinafaultblockregion[J].SeismologyandGeology,5(1):15—28(inChinese).
李钦祖.1980.华北地壳应力场的基本特征[J].地球物理学报,23(4):376—387.LIQin zu.1980.ThefundamentalfeatureofcrustalstressfieldinNorthChina[J].ActaGeophisicaSinica,23(4):376—387(inChinese).
六省(市)震源机制小组.1981.由震源机制解推断苏鲁皖豫地区现代构造应力场[J].地震地质,3(1):19—28.UnitedGroupofFocalMechanismStudy.1981.StudyofrecenttectonicstressfieldofJiangsu Sandong Anhui Henan regionfromfocalmechanismsolutions[J].SeismologyandGeology,3(1):19—28(inChinese).
马宏生,张国民,刘杰,等.2003.中国大陆及其邻区强震活动与活动地块关系研究[J].地学前缘,10(特刊):74—80.MAHong sheng,ZHANGGuo min,LIUJie,etal.2003.Correlationbetweenstrongearthquakeactivityandactive crustalblockinChinamainlandanditsadjacentregions[J].EarthScienceFrontiers,10(Suppl):74—80(in Chinese).
马淑田,张德存.1999.1996年11月9日长江口以东海域MS6.1级地震的震源机制初步研究[A].见:上海市地震局编.上海市的地震与应急:1996年长江口以东海域地震研究文集.北京:地震出版社.32—41.MAShu tian,ZHANGDe cun.1999.PreliminaryresearchonfocalmechanismoftheM6.1earthquakeoccurringinthe EastChinaSeaontheeastoftheYangtzeRiverestuaryonNov.9,1996[A].In:EarthquakeAdministrationof ShanghaiMunicipality(ed).EarthquakeEmergencyResponseofShanghai:theCollectedWorksofResearchon theM6.1EarthquakeintheEastChinaSeaontheEastoftheYangtzeRiverEstuaryonNov.9,1996.Seismo logicalPress,Beijing.32—41(inChinese).
马宗晋.1987.中国大陆的地震层和地震线[A].见:国家地震局地壳应力研究所编.地壳构造与地壳应力文集(一).北京:地震出版社.1—7.MAZong jin.1987.TheseismogeniclayersandlinesinChina smainland[A].In:InstituteofCrustalDynamics,SSB(ed).TheCollectedWorksofCrustalStructureandCrustalStress.SeismologicalPress,Beijing.1—7(in Chinese).
马杏垣主编.1989.中国岩石圈动力学地图集[Z].北京:中国地图出版社.36—44.MAXing yuan(ed).1989.AtlasofLithosphereDynamicsofChina[Z].ChinaCartographicPublishingHouse,Beijing.36—44(inChinese).
魏光兴,周翠英,赵兴兰.1982.华北地区中小地震应力场的优势方向[J].地球物理学报,25(4):333—343.WEIGuang xing,ZHOUCui ying,ZHAOXing lan.1982.TheDominantdirectionsofstressfieldfromminorearth quakesinNorth EasternChina[J].ChineseJournalofGeophysics,25(4):333—343(inChinese).
魏光兴,周翠英,侯海峰,等.1985.聊城-兰考断裂带及其邻区现代地壳应力场与地震活动[J].华北地震科学,3(2):19—29.WEIGuang xing,ZHOUCui ying,HOUHai feng,etal.1985.ModerncruststressfieldandseismicityinLiaocheng LankaoFaultzoneanditsadjacentareas[J].NorthChinaEarthquakeSciences,3(2):19—29(inChinese).
魏光兴,刁守中,周翠英.1993.郯庐带地震活动性研究[M].北京:地震出版社.WEIGuang xing,DIAOShou zhong,ZHOUCui ying.1993.ResearchonSeismicityoftheTanluFaultZone[M].Seis mologicalPress,Beijing(inChinese).
汪素云,许忠淮.1985.中国东部大陆地震构造应力场[J].地震学报,7(1):17—32.WANGSu yun,XUZhong huai.1985.SeismotectonicstressfieldinEastChina[J].ActaSeismologicaSinica,7(1):17—32(inChinese).
吴大铭,张裕明,方仲景,等.1981.论中国郯庐断裂带的活动[J].地震地质,3(4):15—24.WUDa ming,ZHANGYu ming,FANGZhong jing,etal.1981.OntheactivityoftheTancheng LujiangFaultzonein China[J].SeismologyandGeology,3(4):15—24(inChinese).
吴少武,张绍治,刘仲芳.1988.郯庐断裂带江苏段活动特征[J].中国地震,4(3):158—161.WUShao wu,ZHANGShao zhi,LIUZhong fang.1988.ActivitycharacteristicsandearthquakesofJiangsusegment oftheTanluFault[J].EarthquakeResearchinChina,4(3):158—161(inChinese).
许忠淮,汪素云,黄雨蕊,等.1989.由大量地震资料推断的我国大陆构造应力场[J].地球物理学报,32(6):637—647.XUZhong huai,WANGSu yun,HUANGYu rui,etal.1989.ThetectonicstressfieldoftheChinesecontinentdeduced fromagreatnumberofearthquakes[J].ChineseJournalofGeophysics,32(6):636—647(inChinese).
许忠淮,阎明,赵仲和.1983.由多个小震推断的华北地区构造应力场的方向[J].地震学报,5(3):268—279.XUZhong huai,YANMing,ZHAOZhong he.1983.EvaluationofthedirectionoftectonicstressinNorthChinafrom recordeddataofalargenumberofsmallearthquakes[J].ActaSeismologicaSinica,5(3):268—279(inChi nese).
夏瑞良.1985.安徽区域地震应力场的分布特征[J].地震地质,7(3):13—22.XIARui liang.1985.CharacteristicdistributionofregionalseismicstressfieldinAnhuiProvince[J].Seismologyand Geology,7(3):13—22(inChinese).
谢富仁,崔效锋,赵建涛.2004.中国大陆及邻区现代构造应力场分区[J].地球物理学报,47(4):654—662.XIEFu ren,CUIXiao feng,ZHAOJian tao,etal.2004.RegionaldivisionoftherecenttectonicstressfieldinChina andadjacentareas[J].ChineseJournalofGeophysics,47(4):654—662(inChinese).
谢富仁,崔效锋,赵建涛.2003.中国大陆现代构造应力场与强震活动的关系[A].见:谢富仁等编.中国大陆地壳应力环境研究.北京:地质出版社.69—74.XIEFu ren,CUIXiao feng,ZHAOJian tao,etal.2003.Therelationshipbetweenrecenttectonicstressfieldand strongearthquakesinChinesemainland[A].In:XIEFu ren,etal(ed).Researchoncrustalstressstatein Chinaandadjacentarea.GeologicalPublishingHouse,Beijing.69—74(inChinese).
徐杰,马宗晋,陈国光,等.2003.中国大陆东部新构造期北西向断裂带的初步探讨[J].地学前缘,10(特刊):193—198.XUJie,MAZong jin,CHENGuo guang,etal.2003.NWtrendingactivefaultzonesinEasternChinesecontinentin neotectonictime[J].EarthScienceFrontiers,10(Suppl):193—198(inChinese).
鄢家全,时振梁,汪素云,等.1979.中国及邻区现代构造应力场的区域特征[J].地震学报,1(1):9—24.YANJia quan,SHIZhen liang,WANGSu yun,etal.1979.SomefeaturesoftherecenttectonicstressfieldofChin andenvirons[J].ChineseJournalofGeophysics,1(1):9—24(inChinese).
张肇诚,罗兰格,李海华,等.1988.中国震例(1966—1975)[M].北京:地震出版社.144—154.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1988.EarthquakeCasesinChina(1966—1975)[M].Seismologi calPress,Beijing.144—154(inChinese).
张肇诚,罗兰格,李海华,等.1990a.中国震例(1976—1980)[M].北京:地震出版社.286—301,357—384.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1988.EarthquakeCasesinChina(1976—1980)[M].SeismologicalPress,Beijing.286—301,357—384(inChinese).
张肇诚,罗兰格,李海华,等.1990b.中国震例(1981—1985)[M].北京:地震出版社.190—223.ZHANGZhao cheng,LUOLan ge,LIHai hua,etal.1990b.EarthquakeCasesinChina(1981—1985)[M].Seismo logicalPress,Beijing.190—233(inChinese).
张肇诚,郑大林,徐京华.1999a.中国震例(1986—1988)[M].北京:地震出版社.156—173.ZHANGZhao cheng,ZHENGDa lin,XUJing hua.1999.EarthquakeCasesinChina(1986—1988)[M].Seismologi calPress,Beijing.156—173(inChinese).
张肇诚,郑大林,徐京华.1999b.中国震例(1989—1991)[M].北京:地震出版社.176—202.ZHANGZhao cheng,ZHENDa lin,XUjing hua,etal.1990b.EarthquakeCasesinChina(1989—1991)[M].Seis mologicalPress,Beijing.176—202(inChinese).
赵景珍,朱晤.1981.河南林县4.7级地震[J].地震学刊,(1):71—75.ZHAOJing zhen,ZHUWu.1981.TheM4.7EarthquakeofLinxianinHenanProvince[J].Journalofseismology,(1):71—75(inChinese).
周翠英,魏光兴.1987.沂沭带的现代构造应力场与地震活动[J].华北地震科学,5(2):29—39.ZHOUCui ying,WEIGuang xing.1987.RecenttectonicstressfieldandseismicityintheYihe ShuheFaultbelt[J].NorthChinaEarthquakeSciences,5(2):29—39(inChinese).
周翠英,华爱军,蒋海昆,等.2003.以格点尝试法求取的山东地区现代中小地震震源机制解[J].东北地震研究,19(1):1—11.ZHOUCui ying,HUAAi jun,JIANGHai kun,etal.2003.Focalmechanismsolutionsobtainedbygridpointstest methodforcontemporarymoderateandsmallearthquakesinShandongarea[J].SeismologicalResearchofNorth eastChina,19(1):1—11(inChinese).
周翠英,周焕鹏,魏光兴,等.1992.应力场方向的微动态变化及其研究意义[A〕.见:马宗晋主编.大陆多震层研究:国际大陆多震层学术讨论会选集.北京:地震出版社.230—239.ZHOUCui ying,ZHOUHuan peng,WEIGuang xing,etal.1992.Micro variationofstressfieldanditsimplication inresearch[A].In:MAZong jin(ed).StudiesontheContinentalSeismogenicLayer:ProceedingsofWork shoponContinentalSeismogenicLayer.SeismologicalPress,Beijing.230—239(inChinese).
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