鲜水河断裂带全新世活动性研究进展综述
|
摘要
鲜水河断裂带是中国西南山区一条现今活动强烈的大型地震断裂。本文在系统总结前人研究成果的基础上,结合野外地质调查,综述了鲜水河断裂带空间展布特征、活动性质及强度、历史地震地表破裂特征、地震危险性等方面的研究进展。前人研究结果表明,鲜水河断裂带以惠远寺为界可分为两段,进一步可细分为八段;断裂带全新世以来以左旋走滑为主,兼具逆冲性质;整条断裂现今走滑活动速率约为10mm/a左右,垂向变形在2mm/a以内;其中断裂带北西段活动速率为10～20mm/a,南东段则小于10mm/a,一般为5mm/a左右;断裂带地震活动频繁,地震活动性北西段明显高于南东段,强震迁移呈明显的跳跃式特征并具有原地复发性质;断裂带历史地震地表破裂特征与玉树地震所报道的地表破裂特征一致;断裂带地震危险性评价具很多不确定因素,研究程度相对较低。
The Xianshuihe fault zone is a large active seismic-genetic zone in mountainous regions of southwest China.Based on previous studies,in combination with field investigation,the authors systemically summarized the research status about Holocene activity of Xianshuihe fault zone.The fault zone is divided by the Huiyuan Temple into two segments,the northwestern and southeastern segments,which are sub-divided into eight parts.Since the Holocene,the fault has occurred as a strike slip fault with thrust characteristic.The whole strike-slip generally displays an activity rate of about 10mm /a and a vertical deformation of 2mm /a or less.The activity rate is changeable in the fault,e.g.,10 ～ 20mm /a in the northwestern segment but smaller than 10mm /a in the southeastern segment.Accordingly the seismic activity is significantly stronger in the northwestern segment than in the southeastern segment.The earthquakes occurred with skip metastasis and have recurrent nature in situ.The surface rupture characteristics recorded in the historical earthquakes are consistent with those reported in the earthquake surface rupture.The research on seismic risk assessment along the Xianshuihe fault zone needs to be greatly improved.
The Xianshuihe fault zone is a large active seismic-genetic zone in mountainous regions of southwest China.Based on previous studies,in combination with field investigation,the authors systemically summarized the research status about Holocene activity of Xianshuihe fault zone.The fault zone is divided by the Huiyuan Temple into two segments,the northwestern and southeastern segments,which are sub-divided into eight parts.Since the Holocene,the fault has occurred as a strike slip fault with thrust characteristic.The whole strike-slip generally displays an activity rate of about 10mm /a and a vertical deformation of 2mm /a or less.The activity rate is changeable in the fault,e.g.,10 ～ 20mm /a in the northwestern segment but smaller than 10mm /a in the southeastern segment.Accordingly the seismic activity is significantly stronger in the northwestern segment than in the southeastern segment.The earthquakes occurred with skip metastasis and have recurrent nature in situ.The surface rupture characteristics recorded in the historical earthquakes are consistent with those reported in the earthquake surface rupture.The research on seismic risk assessment along the Xianshuihe fault zone needs to be greatly improved.
引文
[1]王连捷,崔军文,周春景,等.汶川5.12地震发震机理的数值模拟[J].地质力学学报,2009,15(2):105～113.WANG Lianjie,CUI Junwen,ZHOU Chunjing,et al.Numerical Modeling for Wenchuan Earthquake Mechanism[J].Journal of Geomechanics,2009,15(2):105～113.
[2]王连捷,周春景,孙东升,等.汶川5.12地震引起的库仑应力变化及其对周边地震活动的影响[J].地质力学学报,2008,14(3):193～200.WANG Lianjie,ZHOU Chunjing,SUN Dongsheng,et al.Coulomb stress changes caused by Wenchuan earthquake and itsinfluence on seismic activity in the adjacent areas[J].Journal of Geomechanics,2008,14(3):193～200.
[3]张永双,雷伟志,石菊松,等.四川5.12地震次生地质灾害的基本特征初析[J].地质力学学报,2008,14(2):109～116.ZHANG Yongshuang,LEI Wei-zhi,SHI Ju-song,et al.General characteristics of 5.12 earthquake-induced geohazards inSichuan[J].Journal of Geomechanics,2008,14(2):109～116.
[4]张永双,石菊松,孙萍,等.汶川地震内外动力耦合及灾害实例[J].地质力学学报,2009,15(2):131～141.ZHANG Yongshuang,SHI Jushong,SUN Ping,et al.Coupling between endogenic and exogenic geological processes in theWenchuan earthquake and example analysis of geohazards[J].Journal of Geomechanics,2009,15(2):131～141.
[5]彭华,马秀敏,姜景捷.山丹地应力监测站体应变仪的地震效应[J].地质力学学报,2008,14(2):97～108.PENG Hua,MA Xiumin,JIANG Jingjie,et al.Analysis of the volume strain data from the Shandan in-situ stress monitoringstation[J].Journal of Geomechanics,2008,14(2):97～108.
[6]彭华,马秀敏,姜景捷.龙门山北端青川断层附近应力测量与断层稳定性[J].地质力学学报,2009,15(2):114～130.PENG Hua,MA Xiumin,JIANG Jing-jie.Stability and stress measurement near the Qinchuan fault in the north LongmenMountains[J].Journal of Geomechanics,2009,15(2):114～130.
[7]谭成轩,孙叶,吴树仁,等.“5.12”汶川MS8.0大地震后关于我国区域地壳稳定性评价的思考[J].地质力学学报,2009,15(2):142～150.TAN Cheng-xuan,SUN Ye,WU Shu-ren,et al.A consideration on regional crustal stability assessment after MS 8.0Wenchuan earthquake in China[J],Journal of Geomechanics,2009,15(2):142～150.
[8]姚鑫,张永双.基于差分干涉雷达的汶川地震同震形变特点[J].地质力学学报,2009,15(2):151～161.YAO Xin,ZHANG Yongshuang.Co-seismic deformation of“5.12”Wenchuan earthquake based on D-InSAR[J].Journalof Geomechanics,2009,15(2):151～161.
[9]马寅生,张永双,胡道功.,等.玉树地震地表破裂与宏观震中[J].地质力学学报,2010,16(2):115～124.MA yinsheng,ZHANG Yongshuang,HU Daogong,et al.The Surface Ruptures And The Macroscopical Epicenter Of YushuMS7.1 Earthquake[J].Journal of Geomechanics,2010,16(2):115～124.
[10]姚鑫,张永双,杨农,等.玉树地震地表变形InSAR观测及初步分析[J].地质力学学报,2010,16(2):129～136.YAO Xin,ZHANG Yong-shuang,Yang Nong,et al.D-InSAR Deformation Observation and Preliminary Analysis of theMS7.1 Yushu Earthquake[J].Journal of Geomechanics,2010,16(2):129～136.
[11]王连捷,崔军文,王薇,等.青海玉树MS 7.1地震发震过程的数值模拟.地质力学学报,2010,16(2):137～145.WANG Lianjie,CUI Junwen,WANG Wei,et al.Numerical modeling for Yushu MS7.1 earthquake mechanism[J].Journal of Geomechanics,2010,16(2):137～145.
[12]罗灼礼,钱洪,闻学泽.鲜水河断裂与圣安德列斯断层的地震地质对比研究[J].四川地震,1987,(4):1～10.QIAN Hong,LUO zhuoli,WEN xuezi.Comparisons study between the Xianshuihe fault and San Andres fault[J].Earthquake research in Sichuan,1990,12(1):22～29.
[13]李天祒主编.鲜水河断裂带及强震危险性评估[M].四川:四川科学技术出版社,1997.LI Tiantiao,et al.The Xianshuihe fault zone and assessment of strong earthquake risk[M].Sichuan:Science andTechnology Press of Sichuan,1997.
[14]周荣军,闻学泽,蔡长星,等.甘孜～玉树断裂带的近代地震与未来地震趋势估计[J].地震地质,1997,(2):115～124.ZHOU Rongjun,WEN Xueze,CAI Changxing,et al.Recent earthquakes and assessment of seismic tendency on theGanzi-Yushu fault zone[J].Seismology and geology,1997,(2):115～124.
[15]Tapponnier.P.,P.Molnar.Active faulting and tectonics of China[J].J.G.R.,1977,82,2905～2930.
[16]WEN Xueze,JIA Jinkang,PAN Mao,et al.Recent slip rates,earthquake recurrence intervals and strong seismic hazardson the northwestern segment of the Xianshuihe fault zone.Earthquake Research in China,1988,2(4):432～451.
[17]Arnold Heim.Earthquake region of Taofu,Chinese Tibet[J].Geological Society of America Bulletin,1934,45:1035～1049.
[18]钱洪,C.R.艾伦,罗灼礼,等.全新世以来鲜水河断裂的活动特征[J].中国地震,1988,4(2):9～18.QIAN Hong,C.R.Allen,LUO zhuoli,et al.The active characteristics of xianshuihe fault in Holocene[J].Earthquakeresearch in China,1988,4(2):9～18.
[19]闻学泽,C.R.艾伦,罗灼礼,等.鲜水河全新世断裂带的分段性、几何特征及其地震构造意义[J].地震学报,1989,11(4):362～371.WEN Xueze,C.R.Allen,LUO Zhuoli.Segmentation,Geometric features and their seismotectonic implications for theHolocene Xianshuihe fault zone[J].Acta Seismologica Sinica,1989,11(4):362～371.
[20]Allen.C.R,LUO Zhuo li,QIAN Hong et al.Field study of a highly active fault zone:The Xianshuihe fault ofsouthwestern China[J].Geol Soc Amer Bull,1991,1(103):1178～1199.
[21]吕弋培,廖华.鲜水河断裂形变场、重力场、磁场动态演化特征与地震[J].四川地震,2001,(3):11～16.LV Yi-pei,LIAO Hua.Dynamic evolution characteristic of deformation,gravity and geo-magnetism fields[J].Earthquakeresearch In Sichuan,2001,(3):11～16.
[22]程万正,杨永林.川滇地块边界构造带形变速率变化与成组强震[J].大地测量与地球动力学,2002,22(4):21～25.CHENG Wanzheng,YANG Yongling.Deformation rate changes of tectonic belts along boundaries of Yunnan-Sichuan blockand their relation to grouped strong earthquakes[J].Crustal deformation and earthquak,2002,22(4):21～25.
[23]乔学军,王琪,杜瑞林.川滇地区活动地块现今地壳形变特征[J].地球物理学报,2004(5):805～811.QIAO Xuejun,WANG Qi,DU Ruilin.GPS;Characteristics of current crustal deformation of active blocks in thesichuan-yunnan region[J].Chinese Journal of Geophysics,2004(5):805～811.
[24]徐锡伟,闻学泽,郑荣章,等.川滇地区活动块体最新构造样式及动力学来源[J].中国科学(D辑),2003,33(s):151～162.XU Xiwei,WEN Xueze,ZHENG Rongzhang,et al.Pattern of latest tectonic motion and dynamics of faulted blocks inYunnan and Sichuan[J].Science in Chian(Serise D),2003,33(sup):151～162.
[25]唐文清,刘宇平,陈智梁,等.鲜水河断裂及两侧地块的GPS监测[J].西南交通大学学报,2005a,40(3):313～317.TANG Wen qing,LIU Yu ping,CHEN Zhi liang.GPS monitoring of Xianshuihe fault and blocks on Its both sides[J].Journal of southwest Jiaotong University,2005a,40(3):313～317
[26]唐文清,陈智梁,刘宇平,等.青藏高原东缘鲜水河断裂与龙门山断裂交会区现今的构造活动[J].地质通报,2005b,24(12):1169～1172.TANG Wenqing,CHEN Zhiliang,LIU Yuping,et al.Present-day tectonics activity in the intersection area of theXianshuihe fault and Longmenshan fault on the eastern margin of the Qinghai-Tibet Plateau[J].Regional geology of China,2005b,24(12):1169～1172.
[27]唐文清,刘宇平,陈智梁,等.基于GPS技术的活动断裂监测——以鲜水河、龙门山断裂为例[J].山地学报,2007,25(1):103～107.TANG Wenqing,LIU Yuping,CHEN Zhiliang,et al.Monitoring of faults activity based on GPS[J].Journal of MountainScience,2007,25(1):103～107.
[28]彭晋川,廖华,顾铁,等基于GPS连续站观测资料的鲜水河断裂运动特征研究[J].四川地震,2007,(4):14～17.PENG Jin-chuan,LIAO Hua,GU Tie.Motion characteristics of the Xianshuihe fault based on observation data of GPScontinuing-run reference stations[J].Earthquake research in Sichuan,2007,(4):14～17.
[29]杨永林,苏琴.鲜水河断裂带现今活动特征研究[J].大地测量与地球动力学,2007,27(6):22～27.YANG Yonglin,SU Qin.Study on present activity characteristics of Xianshuihe fault zone[J].Journal of Geodesy andGeodynamics,2007,27(6):22～27.
[30]唐荣昌,韩渭宾,黄祖智,等.四川活动断裂与地震[M].北京:地震出版社,1993.TANG Rongchang,HAN Weibin,HUANG Zuzhi.Active fault of Sichuan and Earthquake[M].Beijing:EarthquakePress,1993.
[31]潘懋,梁海华,蔡永恩,等.中国川西地区鲜水河断裂和则木河断裂几何学、运动学特征及地震活动性对比研究[J].中国地震,1994,10(1):28～37.PAN Mao,Liang Haihua,Cai Yongen,et al.Comparision between the Xianshuihe fault zone and Zemuhe fult zone[J].Earthquake research in China,1994,10(1):28～37.
[32]唐荣昌,文德华,邓天岗,等.1973炉霍7.9级地震的地裂缝特征及地震原因的初步探讨[J].地球物理学报,1976,19(1):28～37.TANG,Rongchang,WEN Dehua,DENG Tiangang.Preliminary study on characteristics of crack and causation of 1973Luhuo MS 7.9 earthquake[J].Chinese Journal of Geophysics,1994,10(1):28～37.
[33]唐荣昌,钱洪,张文甫,等.道孚6.9级地震的地质构造背景与发震构造条件分析[J].地震地质,1984,6(2):28～37.TANG,Rongchang,QIAN Hong,ZHANG Wenfu,et al.Analysis on tectonic background and earthquake structuralconditions of Daofu MS6.9 earthquake[J].Sesimology and Geology,1984,6(2):28～37.
[34]唐荣昌,韩渭宾.四川活动断裂与地震[M].北京:地震出版社,1993.TANG Rongchang,HAN Weibin,et al.Active fault of Sichuan and Earthquake[M].Beijing:Earthquake Press,1993.
[35]邓天岗主编.鲜水河活动断裂带[M].:四川科学技术出版社,1989.Deng Tiangang,et al.The Xianshuihe active fault zone[M].Sichuan:Science and Technology Press of Sichuan,1997.
[36]周荣军,何玉林,黄祖智.鲜水河断裂带乾宁-康定段的滑动速率与强震复发间隔[J].地震学报,2001b,23(3):22～29.ZHOU Rongjun,HE Yulin,HUANG,Zuzhi,et al.The slip rate and strong earthquake recurrence interval on the Qianning-Kangding segment of the Xianshuihe fault zone[J].Acta seismologica sinica,2001b,23(3):22～29.
[37]孙建中,施顺英,周硕愚等.利用地震矩张量反演鲜水河断裂带现今运动学特征[J].地壳形变与测量,1994,14(4):9～14.SUN Jianzhong,SHI Shunying,ZHOU Shuoyu,et al.Inversion of the present kinematic characteristics of Xianshuihe faultzone from seismic moment tensor[J].Crustal deformation and earthquake,1994,14(4):9～14.
[38]李玶.鲜水河-小江断裂带[M].北京:地震出版社,1993.LI Ping,et al.the Xianshuihe-Xiaojiang fault zone[M].Beijing:Earthquake Press,1993.
[39]钱洪.鲜水河断裂带上潜在震源区的地质学判定[J].四川地震,1988,2:20～28.QIAN Hong.Identification of potential seismic area along the Xianshuihe zone[J].Earthquake research in Sichuan,1988,2:20～28.
[40]钱洪,罗灼礼,闻学泽,等.鲜水河断裂带上特征地震的初步研究[J].中国地震,1990,12(1):22～29.QIAN Hong,LUO zhuoli,WEN xuezi.Preliminary study of characteristic earthquakes in the Xianshuihe fault zone[J].Acta Seismologica Sinica,1990,12(1):22～29.
[41]Schwartz,D.P.ant Coppersmith K.J.,Fault behavior and characteristic earthquakes:example from the Wasatch and SanAndreas fault zones[J].J.Geophys.Res.1984,89,B7,5681～5698.
[42]李天祒,杜其方.鲜水河断裂带炉霍段的水平运动及地震的重复性研究[J].地震地质,1989,11(4):31～42.LI Tiantiao,DU Qifang.Horizontal displacement and earthquake recurrence along Luhuo segment of the Xianshuihe faultzone[J].Sesimology and Geology,1989,11(4):31～42.
[43]钱洪.鲜水河断裂反“多”字型地裂缝带的成因机制[J].地震地质,1983,5(3):75～80.QIAN Hong.The formation of anti xi-type(ξ-type)ground crack zones along the Xianshuihe fault[J].Seismology andGeology,1983,5(3):75～80.
[44]王新民,裴锡瑜.康定-沪定地区主要活断层与地震裂缝[J].四川地震,1998,1～2:46～56.WANG Xinmin,PEI Xiyu.Main active faults and seismic fractures of the Kangding-Luding area[J].Earthquake researchin Sichuan,1998,1～2:46～56.
[45]张永双,马寅生,胡道功,等.玉树地震地表破裂调查与灾后重建避让选址研究[J].地质学报,2010,84(5):593～605.ZHANG Yongshuang,MA Yinsheng,HU Daogong,et al.Investigation and Research on the Surface Rupture of the YushuEarthquake and Reconstruction Site Selection[J].Acta Geologica Sinica,2010,84(5):593～605.
[46]冉洪流,何宏林.鲜水河断裂带北西段不同破裂源强震震级(MS≥6.7)及复发间隔研究[J].地球物理学报,2006,49(1):153～161.RAN Hongliu,HE Honglin.Research on the magnitude and recurrence interval of characterized earthquakes with MagnitudeMS≥6.7 along the northwestern portion of the Xianshuihe fault zone in western Sichuan,China[J].Chinese Journal ofGeophysics,2006,49(1):153～161.
[47]殷跃平,张永双,马寅生,等.青海玉树MS7.1级地震地质灾害主要特征[J].工程地质学报,2010,18(3):289～296.YIN Yueping,ZHANG Yongshuang,MA Yinsheng,et al.Research on major characteristics of geohazards induced by theYushu MS7.1 earthquake.Journal of Engineering Geology,2010,18(3):289～296.
[2]王连捷,周春景,孙东升,等.汶川5.12地震引起的库仑应力变化及其对周边地震活动的影响[J].地质力学学报,2008,14(3):193～200.WANG Lianjie,ZHOU Chunjing,SUN Dongsheng,et al.Coulomb stress changes caused by Wenchuan earthquake and itsinfluence on seismic activity in the adjacent areas[J].Journal of Geomechanics,2008,14(3):193～200.
[3]张永双,雷伟志,石菊松,等.四川5.12地震次生地质灾害的基本特征初析[J].地质力学学报,2008,14(2):109～116.ZHANG Yongshuang,LEI Wei-zhi,SHI Ju-song,et al.General characteristics of 5.12 earthquake-induced geohazards inSichuan[J].Journal of Geomechanics,2008,14(2):109～116.
[4]张永双,石菊松,孙萍,等.汶川地震内外动力耦合及灾害实例[J].地质力学学报,2009,15(2):131～141.ZHANG Yongshuang,SHI Jushong,SUN Ping,et al.Coupling between endogenic and exogenic geological processes in theWenchuan earthquake and example analysis of geohazards[J].Journal of Geomechanics,2009,15(2):131～141.
[5]彭华,马秀敏,姜景捷.山丹地应力监测站体应变仪的地震效应[J].地质力学学报,2008,14(2):97～108.PENG Hua,MA Xiumin,JIANG Jingjie,et al.Analysis of the volume strain data from the Shandan in-situ stress monitoringstation[J].Journal of Geomechanics,2008,14(2):97～108.
[6]彭华,马秀敏,姜景捷.龙门山北端青川断层附近应力测量与断层稳定性[J].地质力学学报,2009,15(2):114～130.PENG Hua,MA Xiumin,JIANG Jing-jie.Stability and stress measurement near the Qinchuan fault in the north LongmenMountains[J].Journal of Geomechanics,2009,15(2):114～130.
[7]谭成轩,孙叶,吴树仁,等.“5.12”汶川MS8.0大地震后关于我国区域地壳稳定性评价的思考[J].地质力学学报,2009,15(2):142～150.TAN Cheng-xuan,SUN Ye,WU Shu-ren,et al.A consideration on regional crustal stability assessment after MS 8.0Wenchuan earthquake in China[J],Journal of Geomechanics,2009,15(2):142～150.
[8]姚鑫,张永双.基于差分干涉雷达的汶川地震同震形变特点[J].地质力学学报,2009,15(2):151～161.YAO Xin,ZHANG Yongshuang.Co-seismic deformation of“5.12”Wenchuan earthquake based on D-InSAR[J].Journalof Geomechanics,2009,15(2):151～161.
[9]马寅生,张永双,胡道功.,等.玉树地震地表破裂与宏观震中[J].地质力学学报,2010,16(2):115～124.MA yinsheng,ZHANG Yongshuang,HU Daogong,et al.The Surface Ruptures And The Macroscopical Epicenter Of YushuMS7.1 Earthquake[J].Journal of Geomechanics,2010,16(2):115～124.
[10]姚鑫,张永双,杨农,等.玉树地震地表变形InSAR观测及初步分析[J].地质力学学报,2010,16(2):129～136.YAO Xin,ZHANG Yong-shuang,Yang Nong,et al.D-InSAR Deformation Observation and Preliminary Analysis of theMS7.1 Yushu Earthquake[J].Journal of Geomechanics,2010,16(2):129～136.
[11]王连捷,崔军文,王薇,等.青海玉树MS 7.1地震发震过程的数值模拟.地质力学学报,2010,16(2):137～145.WANG Lianjie,CUI Junwen,WANG Wei,et al.Numerical modeling for Yushu MS7.1 earthquake mechanism[J].Journal of Geomechanics,2010,16(2):137～145.
[12]罗灼礼,钱洪,闻学泽.鲜水河断裂与圣安德列斯断层的地震地质对比研究[J].四川地震,1987,(4):1～10.QIAN Hong,LUO zhuoli,WEN xuezi.Comparisons study between the Xianshuihe fault and San Andres fault[J].Earthquake research in Sichuan,1990,12(1):22～29.
[13]李天祒主编.鲜水河断裂带及强震危险性评估[M].四川:四川科学技术出版社,1997.LI Tiantiao,et al.The Xianshuihe fault zone and assessment of strong earthquake risk[M].Sichuan:Science andTechnology Press of Sichuan,1997.
[14]周荣军,闻学泽,蔡长星,等.甘孜～玉树断裂带的近代地震与未来地震趋势估计[J].地震地质,1997,(2):115～124.ZHOU Rongjun,WEN Xueze,CAI Changxing,et al.Recent earthquakes and assessment of seismic tendency on theGanzi-Yushu fault zone[J].Seismology and geology,1997,(2):115～124.
[15]Tapponnier.P.,P.Molnar.Active faulting and tectonics of China[J].J.G.R.,1977,82,2905～2930.
[16]WEN Xueze,JIA Jinkang,PAN Mao,et al.Recent slip rates,earthquake recurrence intervals and strong seismic hazardson the northwestern segment of the Xianshuihe fault zone.Earthquake Research in China,1988,2(4):432～451.
[17]Arnold Heim.Earthquake region of Taofu,Chinese Tibet[J].Geological Society of America Bulletin,1934,45:1035～1049.
[18]钱洪,C.R.艾伦,罗灼礼,等.全新世以来鲜水河断裂的活动特征[J].中国地震,1988,4(2):9～18.QIAN Hong,C.R.Allen,LUO zhuoli,et al.The active characteristics of xianshuihe fault in Holocene[J].Earthquakeresearch in China,1988,4(2):9～18.
[19]闻学泽,C.R.艾伦,罗灼礼,等.鲜水河全新世断裂带的分段性、几何特征及其地震构造意义[J].地震学报,1989,11(4):362～371.WEN Xueze,C.R.Allen,LUO Zhuoli.Segmentation,Geometric features and their seismotectonic implications for theHolocene Xianshuihe fault zone[J].Acta Seismologica Sinica,1989,11(4):362～371.
[20]Allen.C.R,LUO Zhuo li,QIAN Hong et al.Field study of a highly active fault zone:The Xianshuihe fault ofsouthwestern China[J].Geol Soc Amer Bull,1991,1(103):1178～1199.
[21]吕弋培,廖华.鲜水河断裂形变场、重力场、磁场动态演化特征与地震[J].四川地震,2001,(3):11～16.LV Yi-pei,LIAO Hua.Dynamic evolution characteristic of deformation,gravity and geo-magnetism fields[J].Earthquakeresearch In Sichuan,2001,(3):11～16.
[22]程万正,杨永林.川滇地块边界构造带形变速率变化与成组强震[J].大地测量与地球动力学,2002,22(4):21～25.CHENG Wanzheng,YANG Yongling.Deformation rate changes of tectonic belts along boundaries of Yunnan-Sichuan blockand their relation to grouped strong earthquakes[J].Crustal deformation and earthquak,2002,22(4):21～25.
[23]乔学军,王琪,杜瑞林.川滇地区活动地块现今地壳形变特征[J].地球物理学报,2004(5):805～811.QIAO Xuejun,WANG Qi,DU Ruilin.GPS;Characteristics of current crustal deformation of active blocks in thesichuan-yunnan region[J].Chinese Journal of Geophysics,2004(5):805～811.
[24]徐锡伟,闻学泽,郑荣章,等.川滇地区活动块体最新构造样式及动力学来源[J].中国科学(D辑),2003,33(s):151～162.XU Xiwei,WEN Xueze,ZHENG Rongzhang,et al.Pattern of latest tectonic motion and dynamics of faulted blocks inYunnan and Sichuan[J].Science in Chian(Serise D),2003,33(sup):151～162.
[25]唐文清,刘宇平,陈智梁,等.鲜水河断裂及两侧地块的GPS监测[J].西南交通大学学报,2005a,40(3):313～317.TANG Wen qing,LIU Yu ping,CHEN Zhi liang.GPS monitoring of Xianshuihe fault and blocks on Its both sides[J].Journal of southwest Jiaotong University,2005a,40(3):313～317
[26]唐文清,陈智梁,刘宇平,等.青藏高原东缘鲜水河断裂与龙门山断裂交会区现今的构造活动[J].地质通报,2005b,24(12):1169～1172.TANG Wenqing,CHEN Zhiliang,LIU Yuping,et al.Present-day tectonics activity in the intersection area of theXianshuihe fault and Longmenshan fault on the eastern margin of the Qinghai-Tibet Plateau[J].Regional geology of China,2005b,24(12):1169～1172.
[27]唐文清,刘宇平,陈智梁,等.基于GPS技术的活动断裂监测——以鲜水河、龙门山断裂为例[J].山地学报,2007,25(1):103～107.TANG Wenqing,LIU Yuping,CHEN Zhiliang,et al.Monitoring of faults activity based on GPS[J].Journal of MountainScience,2007,25(1):103～107.
[28]彭晋川,廖华,顾铁,等基于GPS连续站观测资料的鲜水河断裂运动特征研究[J].四川地震,2007,(4):14～17.PENG Jin-chuan,LIAO Hua,GU Tie.Motion characteristics of the Xianshuihe fault based on observation data of GPScontinuing-run reference stations[J].Earthquake research in Sichuan,2007,(4):14～17.
[29]杨永林,苏琴.鲜水河断裂带现今活动特征研究[J].大地测量与地球动力学,2007,27(6):22～27.YANG Yonglin,SU Qin.Study on present activity characteristics of Xianshuihe fault zone[J].Journal of Geodesy andGeodynamics,2007,27(6):22～27.
[30]唐荣昌,韩渭宾,黄祖智,等.四川活动断裂与地震[M].北京:地震出版社,1993.TANG Rongchang,HAN Weibin,HUANG Zuzhi.Active fault of Sichuan and Earthquake[M].Beijing:EarthquakePress,1993.
[31]潘懋,梁海华,蔡永恩,等.中国川西地区鲜水河断裂和则木河断裂几何学、运动学特征及地震活动性对比研究[J].中国地震,1994,10(1):28～37.PAN Mao,Liang Haihua,Cai Yongen,et al.Comparision between the Xianshuihe fault zone and Zemuhe fult zone[J].Earthquake research in China,1994,10(1):28～37.
[32]唐荣昌,文德华,邓天岗,等.1973炉霍7.9级地震的地裂缝特征及地震原因的初步探讨[J].地球物理学报,1976,19(1):28～37.TANG,Rongchang,WEN Dehua,DENG Tiangang.Preliminary study on characteristics of crack and causation of 1973Luhuo MS 7.9 earthquake[J].Chinese Journal of Geophysics,1994,10(1):28～37.
[33]唐荣昌,钱洪,张文甫,等.道孚6.9级地震的地质构造背景与发震构造条件分析[J].地震地质,1984,6(2):28～37.TANG,Rongchang,QIAN Hong,ZHANG Wenfu,et al.Analysis on tectonic background and earthquake structuralconditions of Daofu MS6.9 earthquake[J].Sesimology and Geology,1984,6(2):28～37.
[34]唐荣昌,韩渭宾.四川活动断裂与地震[M].北京:地震出版社,1993.TANG Rongchang,HAN Weibin,et al.Active fault of Sichuan and Earthquake[M].Beijing:Earthquake Press,1993.
[35]邓天岗主编.鲜水河活动断裂带[M].:四川科学技术出版社,1989.Deng Tiangang,et al.The Xianshuihe active fault zone[M].Sichuan:Science and Technology Press of Sichuan,1997.
[36]周荣军,何玉林,黄祖智.鲜水河断裂带乾宁-康定段的滑动速率与强震复发间隔[J].地震学报,2001b,23(3):22～29.ZHOU Rongjun,HE Yulin,HUANG,Zuzhi,et al.The slip rate and strong earthquake recurrence interval on the Qianning-Kangding segment of the Xianshuihe fault zone[J].Acta seismologica sinica,2001b,23(3):22～29.
[37]孙建中,施顺英,周硕愚等.利用地震矩张量反演鲜水河断裂带现今运动学特征[J].地壳形变与测量,1994,14(4):9～14.SUN Jianzhong,SHI Shunying,ZHOU Shuoyu,et al.Inversion of the present kinematic characteristics of Xianshuihe faultzone from seismic moment tensor[J].Crustal deformation and earthquake,1994,14(4):9～14.
[38]李玶.鲜水河-小江断裂带[M].北京:地震出版社,1993.LI Ping,et al.the Xianshuihe-Xiaojiang fault zone[M].Beijing:Earthquake Press,1993.
[39]钱洪.鲜水河断裂带上潜在震源区的地质学判定[J].四川地震,1988,2:20～28.QIAN Hong.Identification of potential seismic area along the Xianshuihe zone[J].Earthquake research in Sichuan,1988,2:20～28.
[40]钱洪,罗灼礼,闻学泽,等.鲜水河断裂带上特征地震的初步研究[J].中国地震,1990,12(1):22～29.QIAN Hong,LUO zhuoli,WEN xuezi.Preliminary study of characteristic earthquakes in the Xianshuihe fault zone[J].Acta Seismologica Sinica,1990,12(1):22～29.
[41]Schwartz,D.P.ant Coppersmith K.J.,Fault behavior and characteristic earthquakes:example from the Wasatch and SanAndreas fault zones[J].J.Geophys.Res.1984,89,B7,5681～5698.
[42]李天祒,杜其方.鲜水河断裂带炉霍段的水平运动及地震的重复性研究[J].地震地质,1989,11(4):31～42.LI Tiantiao,DU Qifang.Horizontal displacement and earthquake recurrence along Luhuo segment of the Xianshuihe faultzone[J].Sesimology and Geology,1989,11(4):31～42.
[43]钱洪.鲜水河断裂反“多”字型地裂缝带的成因机制[J].地震地质,1983,5(3):75～80.QIAN Hong.The formation of anti xi-type(ξ-type)ground crack zones along the Xianshuihe fault[J].Seismology andGeology,1983,5(3):75～80.
[44]王新民,裴锡瑜.康定-沪定地区主要活断层与地震裂缝[J].四川地震,1998,1～2:46～56.WANG Xinmin,PEI Xiyu.Main active faults and seismic fractures of the Kangding-Luding area[J].Earthquake researchin Sichuan,1998,1～2:46～56.
[45]张永双,马寅生,胡道功,等.玉树地震地表破裂调查与灾后重建避让选址研究[J].地质学报,2010,84(5):593～605.ZHANG Yongshuang,MA Yinsheng,HU Daogong,et al.Investigation and Research on the Surface Rupture of the YushuEarthquake and Reconstruction Site Selection[J].Acta Geologica Sinica,2010,84(5):593～605.
[46]冉洪流,何宏林.鲜水河断裂带北西段不同破裂源强震震级(MS≥6.7)及复发间隔研究[J].地球物理学报,2006,49(1):153～161.RAN Hongliu,HE Honglin.Research on the magnitude and recurrence interval of characterized earthquakes with MagnitudeMS≥6.7 along the northwestern portion of the Xianshuihe fault zone in western Sichuan,China[J].Chinese Journal ofGeophysics,2006,49(1):153～161.
[47]殷跃平,张永双,马寅生,等.青海玉树MS7.1级地震地质灾害主要特征[J].工程地质学报,2010,18(3):289～296.YIN Yueping,ZHANG Yongshuang,MA Yinsheng,et al.Research on major characteristics of geohazards induced by theYushu MS7.1 earthquake.Journal of Engineering Geology,2010,18(3):289～296.
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