河西走廊及邻区大震重复周期估算与未来地震趋势
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摘要
河西走廊是我国中原通往西北地区的重要交通运输要道。受印度板块与欧亚板块于中生代末—新生代早期的碰撞及持续至今的向北推挤作用的远程效应的影响,河西走廊及邻区是现今地壳活动地区,其中地震活动为其主要表现形式。已有地震资料分析显示,公元1555年以来划分为2个平静期和2个活跃期,现在处于1920年以来的第2个活跃期内;而最近100年的第2个活跃期内又可以划分为5个相对平静阶段和5个相对活跃阶段,目前处于2002年以来的第5个活跃阶段内。从大震重复周期分析,区内各断裂带发生7.0～7.5级大地震的时间间隔为2000～3000年左右。结合各断裂带最近一次地震的时间,推测未来100年发生7级以上大震可能性很大的区段是三个墩—松山地区、玉门地区、磁窑口—苦水沟地区和嘉峪关地区;未来100年发生7级以上大震可能性较大的区段是石包城—昌马大坝区段和高台地区。与地震活动相关的研究工作应该在确认活动断裂的基础上加强大震重复周期的研究与分析。
The Hexi corridor,with its particular geographical position,is an important line connecting middle and lower reaches of the Yellow River and NW China.Affected by the late Mesozoic-early Cenozoic collision between Indian Plate and Eurasian Plate and the continuous northward compression the Hexi corridor and its adjacent area occur as a strong Crustal movement zone,as marked by earthquakes.Since 1555AD,two active periods and two quiet periods have been recognized and now is in the second active period since 1920.The second active period in the past 100 years can be divide to five active stages and five quiet stagese,each lasting for 9 ～ 16 years,and now is in the last active stage since 2002.Study of major earthquake cycle indicates that the major earthquakes(MS = 7.0 ～ 7.5) happen at the interval of 2000 ～ 3000 years in the study area.According to the state of every active fault in the recent earthquake,it can be predicted that in the coming 100 years the MS > 7.0 earthquakes most likely appear in San'gedun-Songshan area of Changma active fault zone,Yuemen area in west part of the Northern Qilianshan fault zone,the Ciyaokou-Kushuigou area in the middle part of Northern Qilianshan fault zone and Jiayuguan area of the Jiayuguan active fault,and likely in Shibaocheng-Changmadaba area in eastern part of Altyu tagh active fault and Gaotai area of Gaotaichezhan active fault.The authors suggest that more attention should be paid to active fault and major earthquake cycle in the study related to earthquake movement.
The Hexi corridor,with its particular geographical position,is an important line connecting middle and lower reaches of the Yellow River and NW China.Affected by the late Mesozoic-early Cenozoic collision between Indian Plate and Eurasian Plate and the continuous northward compression the Hexi corridor and its adjacent area occur as a strong Crustal movement zone,as marked by earthquakes.Since 1555AD,two active periods and two quiet periods have been recognized and now is in the second active period since 1920.The second active period in the past 100 years can be divide to five active stages and five quiet stagese,each lasting for 9 ～ 16 years,and now is in the last active stage since 2002.Study of major earthquake cycle indicates that the major earthquakes(MS = 7.0 ～ 7.5) happen at the interval of 2000 ～ 3000 years in the study area.According to the state of every active fault in the recent earthquake,it can be predicted that in the coming 100 years the MS > 7.0 earthquakes most likely appear in San'gedun-Songshan area of Changma active fault zone,Yuemen area in west part of the Northern Qilianshan fault zone,the Ciyaokou-Kushuigou area in the middle part of Northern Qilianshan fault zone and Jiayuguan area of the Jiayuguan active fault,and likely in Shibaocheng-Changmadaba area in eastern part of Altyu tagh active fault and Gaotai area of Gaotaichezhan active fault.The authors suggest that more attention should be paid to active fault and major earthquake cycle in the study related to earthquake movement.
引文
[1]时振梁,环文林,谢原定.河西走廊西部的活动断层与地震,中国活动断裂[C],地震出版社,1982.212～218.SHI Zhen-liang,HUAN Wen-lin and XIE yuan-ding.Active faults and earthquakes in west part of Hexi Corridor[A].Active faults in China.Beijing:Seismological Press,1982.212～218(in Chinese).
[2]向宏发,虢顺民.河西走廊玉门-嘉峪关地区活动断裂的初步研究[C].现代地壳运动研究(5).北京:地震出版社,1990.139～145.XIANG Hong-fa and GUO Shun-min.Preliminary study on active faults in Yumen-Jiayuhuan area of Hexi Corridor[A].In:Institute of Geology,SSB,ed.Research on Recent Crustal Movement(5).Beijing:Seismological Press,1990.139～145(in Chinese).
[3]虢顺民,向宏发,黄昭,等.Tapponnier P and Peltzer G.祁连山-河西走廊断裂带与地震.中法合作活断层对比研究[C].北京:地震出版社,1993,94～102.GUO Shun-min,XIANG Hong-fa,HUANG Zhao,et al.Qilian Mountain-Hexi corridor active fault zone and earthquake.Comparison studing of active faults on China-France cooperation[C].Beijing:Seismological Press,1993.94～102(inChinese).
[4]国家地震局地质研究所,国家地震局兰州地震研究所.祁连山-河西走廊活动断裂系[M].北京:地震出版社,1993.1～340.Institute of Geology,SSB and Lanzhou Institute of Seismology,SSB.Active faults in Qilian mountain and Hexi corrdor[M].Beijing:Seismological Press,1993.1～340(in Chinese).
[5]Pcltzer G,Tapponnier P,Gaudemer Y,等.昌马断裂的晚第四纪地貌断错、滑动速率及大地震重复[M].中法合作活断层对比研究,北京:地震出版社,1993.123～143.Pcltzer G,Tapponnier P,Gaudemer Y,et al.Offsets of late Quaternary morphology,rate of slip,and recurrence of largeearthquakes on the Changma fault,Gansu,China.Comparison studing of active faults on China-France cooperation.Beijing:Seismological Press,1993.123～143(in Chinese).
[6]才树华,向宏发,李伯栋,等.Tapponnier P,Meyer B.祁连山北缘断裂带中段全新世活动特征及其与地震的关系.中法合作活断层对比研究[C].北京:地震出版社,1993.113～122.CAI Shu-hua,XIANG Hong-fa,LI Bo-dong et al.Tapponnier P and Meyer B.Holocene faulting and its relation toearthquake in the central segment of the northern Qilianshan fault zone.Comparison studing of active faults on China-Francecooperation.Beijing:Seismological Press,1993.113～122(in Chinese).
[7]陈文彬,刘百篪,徐锡伟,等.祁连山西段玉门断裂晚第四纪活动特征及相关问题的讨论[J].西北地震学报,1999,21(4):389～394.CHEN Wen-bin,LIU Bai-chi,XU Xi-wei et al.Activity of the Yumen fault,western Qilian mountains,During lateQuaterary and its implication to regional tectonic movements[J].Northwestern Seismological Journal,1999,21(4):389～394(in Chinese with English abstract).
[8]闵伟,张培震,何文贵,等.酒西盆地断层活动特征及古地震研究[J].地震地质,2002,24(1):35～44.MIN Wei,ZHANG Pei-zhen,HE Wen-gui,et al.Reseach on the active faults and paleoearthquakes in the western Jiuquanbasin[J].Seismology and Geology,2002,24(1):27～34(in Chinese with English abstract).
[9]何文贵,刘百篪,袁道阳,等.冷龙岭活动断裂的滑动速率研究[J].西北地震学报,2000,22(1):90～97.HE Wen-gui,LIU Bai-chi,YUAN Dao-yang,et al.Resarch on slip rates of the Lenglongling active fault zone.Northwestern Seismological Journal,2000,22(1):90～97(in Chinese with English abstract).
[10]何文贵,郑文俊,赵广堃，等.2002年12月14日玉门5.9级地震发震构造研究[J].地震地质,2004,26(4):688～697.HE Wen-gui,ZHANG Wen-jun,ZHAO Guang-kun,et al.Study on the seismogenic structure of the Yumen,Gansuprovince 5.9MS earthquake of December 14,2002[J].Seismology and Geology,2004,26(4):688～697(in Chinesewith English abstract).
[11]陈柏林,刘建生,张永双,等.玉门断裂全新世活动特征及其与玉门地震的关系[J].地质论评,2005,51(2):138～142.CHEN Bai-lin,LIU Jian-sheng,ZHANG Yong-shuang,et al.Activity of the Yumen fault during Holocene epoch and itsrelation to Yumen earthquake[J].Geological Review.,2005,51(2):138～142(in Chinese with English abstract).
[12]陈柏林,刘建民,刘建生,等.高台车站断裂全新世活动特征[J].地质学报,2006,80(4):497～507.CHEN Bai-lin,LIU Jian-min,LIU Jian-sheng,WANG Chun-yu,ZHANG Yong-shuang,DONG Cheng and WU Nai-fen.Study on the Activity and Chronology of the Gaotai Railway Station Fault During Holocene Epoch[J].ACTA GeologicaSinica,2006,80(4):497～507(in Chinese with English abstract).
[13]陈柏林,王春宇,宫红良,等.关于河西走廊盆地榆木山北缘断裂晚第四纪活动特征的新认识[J].地质通报,2007,26(8):976～983.CHEN Bai-lin,WANG Chun-yu,GONG Hong-liang,LIU Jian-min,ZHANG Yong-shuang and LIU Jian-sheng.A newunderstanding of the characteristics of Late Quaternary activity of the northern Yumushan marginal fault in the Hexi corridor,northwestern China[J].Geological Bulletin of China,2007,26(8):976～983(in Chinese with English abstract).
[14]陈柏林,刘建生,王春宇,等.阿尔金断裂昌马大坝—宽滩山段全新世活动特征[J].地质学报,2008,82(4):433～440.CHEN Bai-lin,LIU Jian-sheng,WANG Chun-yu,et al.Study on the Activity of the Changmadaba-Kuangtanshan Segmentof Eastern Altyn Tagh Fault During Holocene Epoch[J].ACTA Geologica Sinica,2008,82(4):433～440.
[15]谭成轩,孙叶,吴树仁,等.5.12汶川MS 8.0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 strong earthquake in China[J].Journal of Geomechanics,2009,15(2):142～150.
[16]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 Yong-shuang.Co-seismic deformation of 5.12 Wenchuan earthquake based on D-INSAR[J].Journalof Geomechanics,2009,15(2):151～161.
[17]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 Yong-shuang,LEI Wei-zhi,SHI Ju-song,et al.General characteristics of 5.12 earthquake-induced geo-hazards inSichuan[J].Journal of Geomechanics,2008,14(2):109～116.
[18]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 Yong-shuang,SHI Ju-song,SUN Ping,et al.Coupling between endogenic and exogenic geological processes in theWenchuan earthquake and example analysis of geo-hazards[J].Journal of Geomechanics,2009,15(2):131～141.
[19]王连捷,周春景,孙东生,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 Lian-jie,ZHOU Chun-jing,SUN Dong-sheng,et al.Coulomb stress changes caused by Wenchuan earthquake andits influence on seismic activity in the adjacent area[J].Journal of Geomechanics,2008,14(3):193～200.
[20]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 Lian-jie,CUI Jun-wen,ZHOU Chun-jing,et al.Numerical modeling for Wenchuan earthquake mechanism[J].Journal of Geomechanics,2009,15(2):105～113.
[21]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.
[22]王连捷,崔军文,王薇,等.青海玉树MS7.1地震发震过程的数值模拟[J].地质力学学报,2010,16(2):137～145.WANG Lian-jie,CUI Jun-wen,WANG Wei,et al.Numercal modeling of Yushu MS7.1 earthquake mechanism[J].Journal of Geomechanics,2010,16(2):137～145.
[23]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 Yin-sheng,ZHANG Yong-shuang,HU Dao-gong.et al.The Surface Ruptures And The Macroscopical Epicenter OfYushu MS7.1 Earthquake[J].Journal of Geomechanics,2010,16(2):115～124.
[24]Harks T C,Bucknam R C,Lajoie K R,et al.Modefication of wave cut and faulting-controlled landforms[J].Journal ofGeophysical Research,1984,89(B7):5771～5791.
[25]甘肃省地质矿产局.甘肃省区域地质志[M].北京:地质出版社,1989.1～692.Bureau of Geology and Mineral Resources of Gansu province.Regional geology of Gansu province[M].Beijing:GeologicalPublishing House,1989.1～692(in Chinese with English abstract).
[26]葛肖红,刘俊来.北祁连造山带的形成与背景[J].地学前缘,1999,6(4):223～230.GE Xiao-hong and LIU Jun-lai.Formation and tectonic background of the northern Qilian orogenic belt[J].Earth ScienceFrontiers,1999,6(4):223～230(in Chinese with English abstract).
[27]尹安.喜马拉雅-青藏高原造山带地质演化[J].地球学报,2001,22(3):193～230.YIN An.Geologic evolution of the Himalayan-Tibetan orogen[J].ACTA Geoscientia Sinica,2001,22(3):193～230(in Chinese with English abstract).
[28]朱弟成,潘桂棠,莫宣学,等.印度大陆和欧亚大陆的碰撞时代[J].地球科学进展,2004,19(4):564～571.ZHU Di-cheng,PAN Gui-tang,MO Xuan-xue,DUAN Li-ping and LIAO Zhong-li[J].The age of collision between Indiaand Eurasia.Advances Earth Science,2004,19(4):564～571(in Chinese with English abstract).
[29]莫宣学,赵志丹,周肃,等.印度-亚洲大陆的碰撞时限[J].地质通报,2007,26(10):1240～1244.MO Xuan-xue,ZHAO Zhi-dan,ZHOU Su,et al.On the timing of India-Asia continental collision[J].Geological Bulletinof China,2007,26(10):1240～1244(in Chinese with English abstract).
[30]宋春晖,方小敏,李吉均,等.青藏高原北缘酒西盆地13Ma以来沉积演化与构造隆升[J].中国科学(D辑),2001.31(增刊):155～162.SONG Chun-hui,FANG Xiao-min,LI Ji-jun,et al.Tectonic uplift and sedimentary evolution of the Jiuxi basin in thenorthern margin of the Tibetan plateau since 13Ma B P[J].Science in China(Series D),2001,31(Suppl):155～162(in Chinese).
[31]宋春晖,孙淑荣,方小敏,等.酒西盆地晚新生代沉积物重矿物分析与高原北部隆升[J].沉积学报,2002,20(4):552～559.SONG Chun-hui,SUN Shu-rong,FANG Xiao-min,et al.Analysis of Tectonic Upl if t and Heavy Minerals of Sediments onJiuxi Basin in the Northern Margin of Tibetan Plateau since the Late Cenozoic[J].ACTA Sedimentologica SINICA,2002,20(4):552～559(in Chinese with English abstract).
[32]方小敏,赵志军,李吉均,等.祁连山北缘老君庙背斜晚新生代磁性地层与青藏高原隆升[J].中国科学(D辑),2004,34(2):97～106.FANG Xiao-min,ZHAO Zhi-jun,LI Ji-jun,et al.Magnetostratigraphy of Late Cenozoic Laojunmiao anticline in thenorthern Qilian Mountains and its implications for the northern Tibetan plateau uplift[J].Science in China(Series D),2004,34(2):97～106(in Chinese).
[33]陆洁民,郭召杰,赵泽辉,等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报,2004,10(1):50～61.LU Jie-min,GUO Zhao-jie,ZHAO Ze-hui,et al.Cenozoic Sedimentation Characteristics of Jiuxi Basin and Uplift Historyof Northern Qilian Mountain[J].Geological Journal of China Universities,2004,10(1):50～61(in Chinese withEnglish abstract).
[34]国家地震局兰州地震研究所.昌马活动断裂系[M].北京:地震出版社,1992.1～207.Lanzhou Institute of Seismology,SSB.Active Changma fault zone[M].Beijing:Seismological Press,1992.1～207(inChinese).
[35]陈汉林,杨树锋,肖安成,等.酒泉盆地南缘新生代冲断带的变形特征和变形时间[J].石油与天然气地质,2006,27(4):488～494.CHEN Han-lin,YANG Shu-feng,XIAO An-cheng,et al.Deformation characteristics and time of Cenozoic thrust belt insouthern margin of Jiuquan basin[J].Oil&Gas Geology,2006,27(4):488～494(in Chinese with English abstract).
[36]杨树锋,陈汉林,程晓敢,等.祁连山北缘冲断带的特征和空间变化规律[J].地学前缘,2007,14(5):211～221.YANG Shu-feng,CHEN Han-lin,CHENG Xiao-gan,et al.Deformation characteristics and rules of spatial change for theNorthern Qilianshan thrust belt[J].Earth Science Frontiers,2007,14(5):211～221(in Chinese with Englishabstract).
[37]徐锡伟,Tapponnier P,Woerd J V D,等.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论[J].中国科学(D辑),2003,33(10):967～974.XU Xi-wei,Tapponnier P,Woerd J V D,et al.Late Quaternary sinistral slip rate along the Altyn Tagh fault and itsstructural transformation model[J].Science in China(Serious D),2003,33(10):967～974(in Chinese).
[38]陈正乐,万景林,王小凤,等.阿尔金断裂带8Ma左右的快速走滑及其地质意义[J].地球学报,2002,23(4):295～300.CHEN Zheng-le,WAN Jing-lin,WANG Xiao-feng,et al.Rapid Strike2sl ip of the Altyn Tagh Fault at 8 Ma and ItsGeological Impl ications[J].ACTA Geoscientia Sinica,2002,23(4):295～300(in Chinese with English abstract).
[39]李玉龙,候珍清,康哲民.中国西北陕甘宁青地震区划[M].甘肃人民出版社,1986.LI Yu-long,HOU Zhen-qing and KAN Zhe-min.Seisic zonation in Shanxi,Gansu,Ningxia and Qinghai province,northwestern China[M].Lanzhou:Gansu People Publishing House(in Chinese),1986.
[40]国家地震局阿尔金活动断裂课题组.阿尔金活动断裂带[M].北京:地震出版社,1992.Research Group on the Active Altyn Tagh Fault Zone of SSB.Active Altyn Tagh fault zone[M].Beijing:SeismologicalPress(in Chinese),1992.
[41]Andrews D J,Hanks T C.Scarp degraded by linear diffusion:Inverse solution for age[J].Jour Geophys Res,1985,90(B12):10193～10208.
[42]尤惠川,邓起东,冉勇康.断层崖演化与古地震研究[J].地震地质,2004,26(1):33～45.YOU Hui-chuan,DENG Qi-dong,RAN Yong-kang.Degradation on fault scarp and paleoearthquake research[J].Seismology and Geology,2004,26(1):33～45(in Chinese with English abstract).
[43]何文贵,雷中生,袁道阳,等.新民堡发生7.25级地震[J].西北地震学报,2010,32(1):47～53.HE Wen-gui,LEI Zhong-sheng,YUAN Dao-yang,et al.Disaster characteristics of Huihuipu earthquake in 1785 inYumen,Gansu province,and discussion on its seismogenic structure[J].Northwestern Seismological Journal,2010,32(1):47～53(in Chinese with English abstract).
[2]向宏发,虢顺民.河西走廊玉门-嘉峪关地区活动断裂的初步研究[C].现代地壳运动研究(5).北京:地震出版社,1990.139～145.XIANG Hong-fa and GUO Shun-min.Preliminary study on active faults in Yumen-Jiayuhuan area of Hexi Corridor[A].In:Institute of Geology,SSB,ed.Research on Recent Crustal Movement(5).Beijing:Seismological Press,1990.139～145(in Chinese).
[3]虢顺民,向宏发,黄昭,等.Tapponnier P and Peltzer G.祁连山-河西走廊断裂带与地震.中法合作活断层对比研究[C].北京:地震出版社,1993,94～102.GUO Shun-min,XIANG Hong-fa,HUANG Zhao,et al.Qilian Mountain-Hexi corridor active fault zone and earthquake.Comparison studing of active faults on China-France cooperation[C].Beijing:Seismological Press,1993.94～102(inChinese).
[4]国家地震局地质研究所,国家地震局兰州地震研究所.祁连山-河西走廊活动断裂系[M].北京:地震出版社,1993.1～340.Institute of Geology,SSB and Lanzhou Institute of Seismology,SSB.Active faults in Qilian mountain and Hexi corrdor[M].Beijing:Seismological Press,1993.1～340(in Chinese).
[5]Pcltzer G,Tapponnier P,Gaudemer Y,等.昌马断裂的晚第四纪地貌断错、滑动速率及大地震重复[M].中法合作活断层对比研究,北京:地震出版社,1993.123～143.Pcltzer G,Tapponnier P,Gaudemer Y,et al.Offsets of late Quaternary morphology,rate of slip,and recurrence of largeearthquakes on the Changma fault,Gansu,China.Comparison studing of active faults on China-France cooperation.Beijing:Seismological Press,1993.123～143(in Chinese).
[6]才树华,向宏发,李伯栋,等.Tapponnier P,Meyer B.祁连山北缘断裂带中段全新世活动特征及其与地震的关系.中法合作活断层对比研究[C].北京:地震出版社,1993.113～122.CAI Shu-hua,XIANG Hong-fa,LI Bo-dong et al.Tapponnier P and Meyer B.Holocene faulting and its relation toearthquake in the central segment of the northern Qilianshan fault zone.Comparison studing of active faults on China-Francecooperation.Beijing:Seismological Press,1993.113～122(in Chinese).
[7]陈文彬,刘百篪,徐锡伟,等.祁连山西段玉门断裂晚第四纪活动特征及相关问题的讨论[J].西北地震学报,1999,21(4):389～394.CHEN Wen-bin,LIU Bai-chi,XU Xi-wei et al.Activity of the Yumen fault,western Qilian mountains,During lateQuaterary and its implication to regional tectonic movements[J].Northwestern Seismological Journal,1999,21(4):389～394(in Chinese with English abstract).
[8]闵伟,张培震,何文贵,等.酒西盆地断层活动特征及古地震研究[J].地震地质,2002,24(1):35～44.MIN Wei,ZHANG Pei-zhen,HE Wen-gui,et al.Reseach on the active faults and paleoearthquakes in the western Jiuquanbasin[J].Seismology and Geology,2002,24(1):27～34(in Chinese with English abstract).
[9]何文贵,刘百篪,袁道阳,等.冷龙岭活动断裂的滑动速率研究[J].西北地震学报,2000,22(1):90～97.HE Wen-gui,LIU Bai-chi,YUAN Dao-yang,et al.Resarch on slip rates of the Lenglongling active fault zone.Northwestern Seismological Journal,2000,22(1):90～97(in Chinese with English abstract).
[10]何文贵,郑文俊,赵广堃，等.2002年12月14日玉门5.9级地震发震构造研究[J].地震地质,2004,26(4):688～697.HE Wen-gui,ZHANG Wen-jun,ZHAO Guang-kun,et al.Study on the seismogenic structure of the Yumen,Gansuprovince 5.9MS earthquake of December 14,2002[J].Seismology and Geology,2004,26(4):688～697(in Chinesewith English abstract).
[11]陈柏林,刘建生,张永双,等.玉门断裂全新世活动特征及其与玉门地震的关系[J].地质论评,2005,51(2):138～142.CHEN Bai-lin,LIU Jian-sheng,ZHANG Yong-shuang,et al.Activity of the Yumen fault during Holocene epoch and itsrelation to Yumen earthquake[J].Geological Review.,2005,51(2):138～142(in Chinese with English abstract).
[12]陈柏林,刘建民,刘建生,等.高台车站断裂全新世活动特征[J].地质学报,2006,80(4):497～507.CHEN Bai-lin,LIU Jian-min,LIU Jian-sheng,WANG Chun-yu,ZHANG Yong-shuang,DONG Cheng and WU Nai-fen.Study on the Activity and Chronology of the Gaotai Railway Station Fault During Holocene Epoch[J].ACTA GeologicaSinica,2006,80(4):497～507(in Chinese with English abstract).
[13]陈柏林,王春宇,宫红良,等.关于河西走廊盆地榆木山北缘断裂晚第四纪活动特征的新认识[J].地质通报,2007,26(8):976～983.CHEN Bai-lin,WANG Chun-yu,GONG Hong-liang,LIU Jian-min,ZHANG Yong-shuang and LIU Jian-sheng.A newunderstanding of the characteristics of Late Quaternary activity of the northern Yumushan marginal fault in the Hexi corridor,northwestern China[J].Geological Bulletin of China,2007,26(8):976～983(in Chinese with English abstract).
[14]陈柏林,刘建生,王春宇,等.阿尔金断裂昌马大坝—宽滩山段全新世活动特征[J].地质学报,2008,82(4):433～440.CHEN Bai-lin,LIU Jian-sheng,WANG Chun-yu,et al.Study on the Activity of the Changmadaba-Kuangtanshan Segmentof Eastern Altyn Tagh Fault During Holocene Epoch[J].ACTA Geologica Sinica,2008,82(4):433～440.
[15]谭成轩,孙叶,吴树仁,等.5.12汶川MS 8.0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 strong earthquake in China[J].Journal of Geomechanics,2009,15(2):142～150.
[16]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 Yong-shuang.Co-seismic deformation of 5.12 Wenchuan earthquake based on D-INSAR[J].Journalof Geomechanics,2009,15(2):151～161.
[17]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 Yong-shuang,LEI Wei-zhi,SHI Ju-song,et al.General characteristics of 5.12 earthquake-induced geo-hazards inSichuan[J].Journal of Geomechanics,2008,14(2):109～116.
[18]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 Yong-shuang,SHI Ju-song,SUN Ping,et al.Coupling between endogenic and exogenic geological processes in theWenchuan earthquake and example analysis of geo-hazards[J].Journal of Geomechanics,2009,15(2):131～141.
[19]王连捷,周春景,孙东生,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 Lian-jie,ZHOU Chun-jing,SUN Dong-sheng,et al.Coulomb stress changes caused by Wenchuan earthquake andits influence on seismic activity in the adjacent area[J].Journal of Geomechanics,2008,14(3):193～200.
[20]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 Lian-jie,CUI Jun-wen,ZHOU Chun-jing,et al.Numerical modeling for Wenchuan earthquake mechanism[J].Journal of Geomechanics,2009,15(2):105～113.
[21]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.
[22]王连捷,崔军文,王薇,等.青海玉树MS7.1地震发震过程的数值模拟[J].地质力学学报,2010,16(2):137～145.WANG Lian-jie,CUI Jun-wen,WANG Wei,et al.Numercal modeling of Yushu MS7.1 earthquake mechanism[J].Journal of Geomechanics,2010,16(2):137～145.
[23]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 Yin-sheng,ZHANG Yong-shuang,HU Dao-gong.et al.The Surface Ruptures And The Macroscopical Epicenter OfYushu MS7.1 Earthquake[J].Journal of Geomechanics,2010,16(2):115～124.
[24]Harks T C,Bucknam R C,Lajoie K R,et al.Modefication of wave cut and faulting-controlled landforms[J].Journal ofGeophysical Research,1984,89(B7):5771～5791.
[25]甘肃省地质矿产局.甘肃省区域地质志[M].北京:地质出版社,1989.1～692.Bureau of Geology and Mineral Resources of Gansu province.Regional geology of Gansu province[M].Beijing:GeologicalPublishing House,1989.1～692(in Chinese with English abstract).
[26]葛肖红,刘俊来.北祁连造山带的形成与背景[J].地学前缘,1999,6(4):223～230.GE Xiao-hong and LIU Jun-lai.Formation and tectonic background of the northern Qilian orogenic belt[J].Earth ScienceFrontiers,1999,6(4):223～230(in Chinese with English abstract).
[27]尹安.喜马拉雅-青藏高原造山带地质演化[J].地球学报,2001,22(3):193～230.YIN An.Geologic evolution of the Himalayan-Tibetan orogen[J].ACTA Geoscientia Sinica,2001,22(3):193～230(in Chinese with English abstract).
[28]朱弟成,潘桂棠,莫宣学,等.印度大陆和欧亚大陆的碰撞时代[J].地球科学进展,2004,19(4):564～571.ZHU Di-cheng,PAN Gui-tang,MO Xuan-xue,DUAN Li-ping and LIAO Zhong-li[J].The age of collision between Indiaand Eurasia.Advances Earth Science,2004,19(4):564～571(in Chinese with English abstract).
[29]莫宣学,赵志丹,周肃,等.印度-亚洲大陆的碰撞时限[J].地质通报,2007,26(10):1240～1244.MO Xuan-xue,ZHAO Zhi-dan,ZHOU Su,et al.On the timing of India-Asia continental collision[J].Geological Bulletinof China,2007,26(10):1240～1244(in Chinese with English abstract).
[30]宋春晖,方小敏,李吉均,等.青藏高原北缘酒西盆地13Ma以来沉积演化与构造隆升[J].中国科学(D辑),2001.31(增刊):155～162.SONG Chun-hui,FANG Xiao-min,LI Ji-jun,et al.Tectonic uplift and sedimentary evolution of the Jiuxi basin in thenorthern margin of the Tibetan plateau since 13Ma B P[J].Science in China(Series D),2001,31(Suppl):155～162(in Chinese).
[31]宋春晖,孙淑荣,方小敏,等.酒西盆地晚新生代沉积物重矿物分析与高原北部隆升[J].沉积学报,2002,20(4):552～559.SONG Chun-hui,SUN Shu-rong,FANG Xiao-min,et al.Analysis of Tectonic Upl if t and Heavy Minerals of Sediments onJiuxi Basin in the Northern Margin of Tibetan Plateau since the Late Cenozoic[J].ACTA Sedimentologica SINICA,2002,20(4):552～559(in Chinese with English abstract).
[32]方小敏,赵志军,李吉均,等.祁连山北缘老君庙背斜晚新生代磁性地层与青藏高原隆升[J].中国科学(D辑),2004,34(2):97～106.FANG Xiao-min,ZHAO Zhi-jun,LI Ji-jun,et al.Magnetostratigraphy of Late Cenozoic Laojunmiao anticline in thenorthern Qilian Mountains and its implications for the northern Tibetan plateau uplift[J].Science in China(Series D),2004,34(2):97～106(in Chinese).
[33]陆洁民,郭召杰,赵泽辉,等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报,2004,10(1):50～61.LU Jie-min,GUO Zhao-jie,ZHAO Ze-hui,et al.Cenozoic Sedimentation Characteristics of Jiuxi Basin and Uplift Historyof Northern Qilian Mountain[J].Geological Journal of China Universities,2004,10(1):50～61(in Chinese withEnglish abstract).
[34]国家地震局兰州地震研究所.昌马活动断裂系[M].北京:地震出版社,1992.1～207.Lanzhou Institute of Seismology,SSB.Active Changma fault zone[M].Beijing:Seismological Press,1992.1～207(inChinese).
[35]陈汉林,杨树锋,肖安成,等.酒泉盆地南缘新生代冲断带的变形特征和变形时间[J].石油与天然气地质,2006,27(4):488～494.CHEN Han-lin,YANG Shu-feng,XIAO An-cheng,et al.Deformation characteristics and time of Cenozoic thrust belt insouthern margin of Jiuquan basin[J].Oil&Gas Geology,2006,27(4):488～494(in Chinese with English abstract).
[36]杨树锋,陈汉林,程晓敢,等.祁连山北缘冲断带的特征和空间变化规律[J].地学前缘,2007,14(5):211～221.YANG Shu-feng,CHEN Han-lin,CHENG Xiao-gan,et al.Deformation characteristics and rules of spatial change for theNorthern Qilianshan thrust belt[J].Earth Science Frontiers,2007,14(5):211～221(in Chinese with Englishabstract).
[37]徐锡伟,Tapponnier P,Woerd J V D,等.阿尔金断裂带晚第四纪左旋走滑速率及其构造运动转换模式讨论[J].中国科学(D辑),2003,33(10):967～974.XU Xi-wei,Tapponnier P,Woerd J V D,et al.Late Quaternary sinistral slip rate along the Altyn Tagh fault and itsstructural transformation model[J].Science in China(Serious D),2003,33(10):967～974(in Chinese).
[38]陈正乐,万景林,王小凤,等.阿尔金断裂带8Ma左右的快速走滑及其地质意义[J].地球学报,2002,23(4):295～300.CHEN Zheng-le,WAN Jing-lin,WANG Xiao-feng,et al.Rapid Strike2sl ip of the Altyn Tagh Fault at 8 Ma and ItsGeological Impl ications[J].ACTA Geoscientia Sinica,2002,23(4):295～300(in Chinese with English abstract).
[39]李玉龙,候珍清,康哲民.中国西北陕甘宁青地震区划[M].甘肃人民出版社,1986.LI Yu-long,HOU Zhen-qing and KAN Zhe-min.Seisic zonation in Shanxi,Gansu,Ningxia and Qinghai province,northwestern China[M].Lanzhou:Gansu People Publishing House(in Chinese),1986.
[40]国家地震局阿尔金活动断裂课题组.阿尔金活动断裂带[M].北京:地震出版社,1992.Research Group on the Active Altyn Tagh Fault Zone of SSB.Active Altyn Tagh fault zone[M].Beijing:SeismologicalPress(in Chinese),1992.
[41]Andrews D J,Hanks T C.Scarp degraded by linear diffusion:Inverse solution for age[J].Jour Geophys Res,1985,90(B12):10193～10208.
[42]尤惠川,邓起东,冉勇康.断层崖演化与古地震研究[J].地震地质,2004,26(1):33～45.YOU Hui-chuan,DENG Qi-dong,RAN Yong-kang.Degradation on fault scarp and paleoearthquake research[J].Seismology and Geology,2004,26(1):33～45(in Chinese with English abstract).
[43]何文贵,雷中生,袁道阳,等.新民堡发生7.25级地震[J].西北地震学报,2010,32(1):47～53.HE Wen-gui,LEI Zhong-sheng,YUAN Dao-yang,et al.Disaster characteristics of Huihuipu earthquake in 1785 inYumen,Gansu province,and discussion on its seismogenic structure[J].Northwestern Seismological Journal,2010,32(1):47～53(in Chinese with English abstract).
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