2018年5月松原M_S5.7地震序列发震断层及应力场特征
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摘要
利用双差定位方法对2018年松原M_S5.7地震序列中ML≥1.0地震重新定位,之后使用CAP方法求解松原M_S5.7地震序列中强地震的震源机制解,再借助MSATSI软件包反演得到松原地区的区域应力场。综合分析以上研究结果得到如下结论:(1)松原M_S5.7地震序列发生在NW走向的第二松花江断裂与NE走向的扶余—肇东断裂交会处,将地震精定位结果沿两条断层走向作剖面分析,NW向剖面主轴长度约为5 km,震中分布均匀,NE向剖面主轴长度亦约为5 km,震中呈倾向NE的高倾角分布;(2)该序列中的4次ML≥3.7地震的震源机制解具有良好的一致性:节面Ⅰ走向为NE向,节面Ⅱ走向为NW向,均为高倾角走滑断层。中强地震的震源机制节面解与第二松花江断裂性质基本一致,由此推断第二松花江断裂是本次松原地震的发震断层;(3)松原地区的主压应力方位角为N86°E,倾角为7°,主张应力方位角为N24°E,倾角为71°。松原地区的区域应力场既受到大尺度的板块构造运动的控制,又受到区域构造运动的影响。在太平洋板块对北东亚板块向西俯冲作用下,东北地区产生了近EW向的主压应力,受周边地质构造控制,松辽盆地内NE向断裂与NW向断裂交会处易发生走滑型地震,2018年松原M_S5.7地震正是在这种构造作用控制下发生的中强地震。
In recent years,moderate-strong earthquakes in Songyuan area of Jilin Province are active. Studying the fault structure and stress field characteristics of the earthquake sequence in Songyuan area is of great significance for scientific understanding of the earthquakepreserving environment in Northeast China and earthquake prevention. The ML≥1.0 earthquakes are relocated by the method of double difference relocation, the focal mechanism solutions of the strong earthquakes are determined by the CAP method, and the stress field is determined by the FMSI method. According to the results,we realize that:① The Songyuan MS5.7 earthquake sequence occurred at the intersection of the Second Songhuajiang fault trending NW and Fuyu-Zhaodong fault trending NE. The results of earthquakes relocation are analyzed along the two faults. The length of the NW axis is about 5 km, the same as to NE axis.The epicenters on the profile of NW axis have a high inclination distribution, while the NE axis is uniform. ② The focal mechanism solutions of four ML≥3.7 earthquakes are all of strike-slip type with high dip angles and good consistency:The strike of nodal plane Ⅰ is NE,and the other is NW. The focal mechanisms of the moderate-strong earthquakes are basically consistent with the Second Songhuajiang fault,and it is concluded that the Second Songhuajiang fault is the seismogenic fault of the Songyuan MS5.7 earthquake;③ The principal compressive stress azimuth and the inclination angle of Songyuan area are N86°E and 7°,respectively,and the principal tensile stress azimuth and the inclination angle are N24°E and 71°,respectively. The regional stress field in Songyuan area is controlled by both large-scale plate tectonic movement and regional tectonic movement. Under the westward subduction of the Pacific Plate,the Northeast Asia Plate's principal compressive stress near the EW direction is generated,which is controlled by the surrounding geological structure. The strike-slip type earthquake is prone to occur at the intersection of the NE-trending fault and the NW-trending fault in the Songliao basin,while the 2018 Songyuan MS5.7 earthquake is a moderate-strong earthquake that occurred under the control of such tectonic action.
In recent years,moderate-strong earthquakes in Songyuan area of Jilin Province are active. Studying the fault structure and stress field characteristics of the earthquake sequence in Songyuan area is of great significance for scientific understanding of the earthquakepreserving environment in Northeast China and earthquake prevention. The ML≥1.0 earthquakes are relocated by the method of double difference relocation, the focal mechanism solutions of the strong earthquakes are determined by the CAP method, and the stress field is determined by the FMSI method. According to the results,we realize that:① The Songyuan MS5.7 earthquake sequence occurred at the intersection of the Second Songhuajiang fault trending NW and Fuyu-Zhaodong fault trending NE. The results of earthquakes relocation are analyzed along the two faults. The length of the NW axis is about 5 km, the same as to NE axis.The epicenters on the profile of NW axis have a high inclination distribution, while the NE axis is uniform. ② The focal mechanism solutions of four ML≥3.7 earthquakes are all of strike-slip type with high dip angles and good consistency:The strike of nodal plane Ⅰ is NE,and the other is NW. The focal mechanisms of the moderate-strong earthquakes are basically consistent with the Second Songhuajiang fault,and it is concluded that the Second Songhuajiang fault is the seismogenic fault of the Songyuan MS5.7 earthquake;③ The principal compressive stress azimuth and the inclination angle of Songyuan area are N86°E and 7°,respectively,and the principal tensile stress azimuth and the inclination angle are N24°E and 71°,respectively. The regional stress field in Songyuan area is controlled by both large-scale plate tectonic movement and regional tectonic movement. Under the westward subduction of the Pacific Plate,the Northeast Asia Plate's principal compressive stress near the EW direction is generated,which is controlled by the surrounding geological structure. The strike-slip type earthquake is prone to occur at the intersection of the NE-trending fault and the NW-trending fault in the Songliao basin,while the 2018 Songyuan MS5.7 earthquake is a moderate-strong earthquake that occurred under the control of such tectonic action.
引文
房立华,吴建平,王未来,吕作勇,王长在,杨婷,蔡妍.2013.四川芦山MS7.0级地震及其余震序列重定位[J].科学通报,58(20):1901-1909.Fang L H,Wu J P,Wang W L,LüZ Y,Wang C Z,Yang T,Cai Y.2013.Relocation of the mainshock and aftershock sequences of MS7.0 Sichuan Lushan earthquake[J].Chinese Science Bulletin,58(28/29):3451-3459.
傅维洲,贺日政.1999.松辽盆地及周边地带地震构造特征[J].世界地质,18(2):95-100.Fu W Z,He R Z.1999.Structural characteristics of earthquakes in Songliao Basin and its peripheral regions[J].World Geology,18(2):95-100(in Chinese).
韩立波,蒋长胜,包丰.2012.2010年河南太康MS4.6地震序列震源参数的精确确定[J].地球物理学报,55(9):2973-2981.Han L B,Jiang C S,Bao F.2012.Source parameter determination of 2010 Taikang MS4.6 earthquake sequences[J].Chinese Journal of Geophysics,55(9):2973-2981(in Chinese).
胡望水,吕炳全,张文军,毛治国,冷军,官大勇.2005.松辽盆地构造演化及成盆动力学探讨[J].地质科学,40(1):16-31.Hu W S,LüB Q,Zhang W J,Mao Z G,Leng J,Guan D Y.2005.An approach to tectonic evolution and dynamics of the Songliao Basin[J].Chinese Journal of Geology,40(1):16-31(in Chinese).
黄媛,吴建平,张天中,张东宁.2008.汶川8.0级大地震及其余震序列重定位研究[J].中国科学:D辑,38(10):1242-1249.Huang Y,Wu J P,Zhang T Z,Zhang D N.2008.Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence[J].Science in China:Series D,51(2):1703-1711.
李恩泽,刘财,张良怀,曾昭发.2012.松辽盆地地震构造与地震活动相关性研究[J].地球物理学进展,27(4):1337-1349.Li E Z,Liu C,Zhang L H,Zeng Z F.2012.The correlation of structure and earthquake in Songliao Basin[J].Progress in Geophysics,27(4):1337-1349(in Chinese).
李圣强,陈棋福,赵里,朱露培,高金哲,李闽峰,刘桂平,王斌.2013.2011年5月中国东北MW5.7深震的非同寻常震源机制:区域波形反演与成因探讨[J].地球物理学报,56(9):2959-2970.Li S Q,Chen Q F,Zhao L,Zhu L P,Gao J Z,Li M F,Liu G P,Wang B.2013.Anomalous focal mechanism of the May 2011MW5.7 deep earthquake in northeastern China:Regional waveform inversion and possible mechanism[J].Chinese Journal of Geophysics,56(9):2959-2970(in Chinese).
李志田,赵成弼,郭孟习.2002.第二松花江断裂活动性剖析[J].吉林地质,21(1/2):15-19.Li Z T,Zhao C B,Guo M X.2002.Analysis of the Second Songhua River fault activities[J].Jilin Geology,21(1/2):15-19(in Chinese).
刘权锋,盛俭,卢滔,张洪艳,盘晓东.2017.扶余/松原-肇东断裂研究综述[J].防灾科技学院学报,19(3):8-16.Liu Q F,Sheng J,Lu T,Zhang H Y,Pan X D.2017.Research status of Fuyu/Songyuan-Zhaodong fault[J].Journal of Institute of Disaster Prevention,19(3):8-16(in Chinese).
罗钧,赵翠萍,周连庆.2014.川滇块体及周边区域现今震源机制和应力场特征[J].地震地质,36(2):405-421.Luo J,Zhao C P,Zhou L Q.2014.Characteristics of focal mechanisms and stress field of the Chuan-Dian rhombic block and its adjacent regions[J].Seismology and Geology,36(2):405-421(in Chinese).
罗艳,倪四道,曾祥方,郑勇,陈祺福,陈颙.2010.汶川地震余震区东北端一个余震序列的地震学研究[J].中国科学:地球科学,40(6):677-687.Luo Y,Ni S D,Zeng X F,Zheng Y,Chen Q F,Chen Y.2010.A shallow aftershock sequence in the north-eastern end of the Wenchuan earthquake aftershock zone[J].Science China Earth Sciences,53(11):1655-1664.
罗艳,倪四道,曾祥方,谢军,陈颙,龙锋.2011.一个发生在沉积盖层里的破坏性地震:2010年1月31日四川遂宁-重庆潼南地震[J].科学通报,56(2):147-152.Luo Y,Ni S D,Zeng X F,Xie J,Chen Y,Long F.2011.The M5.0 Suining-Tongnan(China)earthquake of 31 January 2010:A destructive earthquake occurring in sedimentary cover[J].Chinese Science Bulletin,56(6):521-525.
孙文斌,和跃时.2004.中国东北地区地震活动特征及其与日本海板块俯冲的关系[J].地震地质,26(1):122-132.Sun W B,He Y S.2004.The feature of seismicity in Northeast China and its relation to the subduction of the Japan Sea Plate[J].Seismology and Geology,26(1):122-132(in Chinese).
王勤彩,王中平,张金川,李君,陈章立.2015.2010年4月玉树MS7.3地震序列的断层结构[J].地球物理学报,58(6):1931-1940.Wang Q C,Wang Z P,Zhang J C,Li J,Chen Z L.2015.Fault structure of MS7.3 Yushu earthquake sequence in April,2010[J].Chinese Journal of Geophysics,58(6):1931-1940(in Chinese).
王未来,吴建平,房立华,王长在.2012.2010年玉树MS7.1地震及其余震的双差定位研究[J].中国科学:地球科学,42(7):1037-1046.Wang W L,Wu J P,Fang L H,Wang C Z.2012.Relocation of the Yushu MS7.1 earthquake and its aftershocks in 2010 from HypoDD[J].Science China Earth Sciences,56(2):182-191.
王未来,吴建平,房立华,来贵娟.2014.2014年云南鲁甸MS6.5地震序列的双差定位[J].地球物理学报,57(9):3042-3051.Wang W L,Wu J P,Fang L H,Lai G J.2014.Double difference location of the Ludian MS6.5 earthquake sequences in Yunnan Province in 2014[J].Chinese Journal of Geophysics,57(9):3042-3051(in Chinese).
吴微微,杨建思,苏金蓉,杜文康,高瑜,郑钰,田宝峰,刘莎,吴朋.2014.2013年吉林前郭-乾安震源区中强地震矩张量反演与区域孕震环境研究[J].地球物理学报,57(8):2541-2554.Wu W W,Yang J S,Su J R,Du W K,Gao Y,Zheng Y,Tian B F,Liu S,Wu P.2014.Moment inversion of moderate earthquakes and seismogenic environment in Qianguo-Qian’an source region,2013,Jilin Province[J].Chinese Journal of Geophysics,57(8):2541-2554(in Chinese).
许忠淮.2001.东亚地区现今构造应力图的编制[J].地震学报,23(5):492-501.Xu Z H.2001.A present-day tectonic stress map for eastern Asia region[J].Acta Seismologica Sinica,23(5):492-501(in Chinese).
杨宝俊,穆石敏,金旭,刘财.1996.中国满洲里-绥芬河地学断面地球物理综合研究[J].地球物理学报,39(6):772-782.Yang B J,Mu S M,Jin X,Liu C.1996.Synthesized study on the geophysics of Manzhouli-Suifenhe geoscience transect China[J].Chinese Journal of Geophysics,39(6):772-782(in Chinese).
曾祥方,罗艳,韩立波,石耀霖.2013.2013年4月20日四川芦山MS7.0地震:一个高角度逆冲地震[J].地球物理学报,56(4):1418-1424.Zeng X F,Luo Y,Han L B,Shi Y L.2013.The Lushan MS7.0 earthquake on 20 April 2013:A high-angle thrust event[J].Chinese Journal of Geophysics,56(4):1418-1424(in Chinese).
张凤鸣,张亚江,许晓艳,张天雷,张震.2007.日本海西部-中国东北深震区俯冲运动对东北地区浅源地震的动力作用[J].东北地震研究,23(1):33-39.Zhang F M,Zhang Y J,Xu X Y,Zhang T L,Zhang Z.2007.Dynamic action on the subduction movement of the west part of Japan sea-deep focus earthquake region in northeast area of China to the shallow source earthquake in northeast area[J].Seismological Research of Northeast China,23(1):33-39(in Chinese).
张慧,焦明若,刘峡.2012.太平洋板块俯冲对中国东北深浅震影响机理的数值模拟[J].地震,32(2):135-144.Zhang H,Jiao M R,Liu X.2012.Numerical simulations of the influencing mechanism of the Pacific Plate subduction to NEChina on deep and shallow earthquakes[J].Earthquake,32(2):135-144(in Chinese).
张萍,孙文福,苗春兰,高艳玲,邹向荣.2009.东北地区中强地震震源机制解分析[J].地震地磁观测研究,30(1):12-19.Zhang P,Sun W F,Miao C L,Gao Y L,Zou X R.2009.Analysis of focal mechanism solution of moderately strong earthquakes in Northeast China[J].Seismological and Geomagnetic Observation and Research,30(1):12-19(in Chinese).
郑秀芬,欧阳飚,张东宁,姚志祥,梁建宏,郑洁.2009.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑[J].地球物理学报,52(5):1412-1417.Zheng X F,Ouyang B,Zhang D N,Yao Z X,Liang J H,Zheng J.2009.Technical system construction of data backup center for China seismograph network and the data support to researches on the Wenchuan earthquake[J].Chinese Journal of Geophysics,52(5):1412-1417(in Chinese).
郑勇,马宏生,吕坚,倪四道,李迎春,韦生吉.2009.汶川地震强余震(MS≥5.6)的震源机制解及其与发震构造的关系[J].中国科学:D辑,39(4):413-426.Zheng Y,Ma H S,LüJ,Ni S D,Li Y C,Wei S J.2009.Source mechanism of strong aftershocks(MS≥5.6)of the2008-05-12 Wenchuan earthquake and the implication for seismotectonics[J].Science in China:Series D,52(6):739-753.
Artemieva I M,Mooney W D.2001.Thermal thickness and evolution of Precambrian lithosphere:A global study[J].J Geophys Res,106(B8):16387-16414.
Gephart J W,Forsyth D W.1984.An improved method for determining the regional stress tensor using earthquake focal mechanism data:Application to the San Fernando earthquake sequence[J].J Geophys Res,89(B11):9305-9320.
Gudmundssonó,Sambridge M.1998.A regionalized upper mantle(RUM)seismic model[J].J Geophys Res,103(B4):7121-7136.
Guo Z,Chen Y J,Ning J Y,Feng Y G,Grand S P,Niu F L,Kawakatsu H,Tanaka S,Obayashi M,Ni J.2015.High resolution 3-D crustal structure beneath NE China from joint inversion of ambient noise and receiver functions using NECESSArray data[J].Earth Planet Sci Lett,416:1-11.
Hardebeck J L,Michael A J.2006.Damped regional-scale stress inversions methodology and examples for southern California and the Coalinga aftershock sequence[J].J Geophys Res,111(B11):B11310.
Helmberger D V,Engen G R.1980.Modeling the long-period body waves from shallow earthquakes at regional ranges[J].Bull Seismol Soc Am,70(5):1699-1714.
Pasyanos M E,Masters T E,Laske G,Ma Z.2014.LITHO1.0:An updated crust and lithospheric model of the Earth[J].J Geophys Res,119(3):2153-2173.
Lund B,Townend J.2007.Calculating horizontal stress orientations with full or partial knowledge of the tectonic stress tensor[J].Geophys J Int,170(3):1328-1335.
Martínez-Garzón P,Kwiatek G,Sone H,Bohnhoff M,Dresen G,Hartline C.2014.Spatiotemporal changes,faulting regimes,and source parameters of induced seismicity:A case study from the Geysers geothermal field[J].J Geophys Res,119(11):8378-8396.
Michael A J.1984.Determination of stress from slip data:Faults and folds[J].J Geophys Res,89(B13):11517-11526.
Waldhauser F,Ellsworth W L.2000.A double-difference earthquake location algorithm:Method and application to the northern Hayward fault,California[J].Bull Seismol Sco Am,90(6):1353-1368.
Waldhauser F,Ellsworth W L.2002.Fault structure and mechanics of the Hayward fault,California,from double-difference earthquake locations[J].J Geophys Res,107(B3):ESE 3-1-ESE 3-15.
Wan Y G.2010.Contemporary tectonic stress field in China[J].Earthquake Science,23(4):377-386.
Zhao L S,Helmberger D V.1994.Source estimation from broad-band regional seismograms[J].Bull Seismol Soc Am,84(1):91-104.
Zhu L P,Helmberger D V.1996.Advancement in source estimation techniques using broadband regional seismograms[J].Bull Seismol Soc Am,86(5):1634-1641.
Zhu L P,Rivera L A.2002.A note on the dynamic and static displacements from a point source in multilayered media[J].Geophys J Int,148(3):619-627.
傅维洲,贺日政.1999.松辽盆地及周边地带地震构造特征[J].世界地质,18(2):95-100.Fu W Z,He R Z.1999.Structural characteristics of earthquakes in Songliao Basin and its peripheral regions[J].World Geology,18(2):95-100(in Chinese).
韩立波,蒋长胜,包丰.2012.2010年河南太康MS4.6地震序列震源参数的精确确定[J].地球物理学报,55(9):2973-2981.Han L B,Jiang C S,Bao F.2012.Source parameter determination of 2010 Taikang MS4.6 earthquake sequences[J].Chinese Journal of Geophysics,55(9):2973-2981(in Chinese).
胡望水,吕炳全,张文军,毛治国,冷军,官大勇.2005.松辽盆地构造演化及成盆动力学探讨[J].地质科学,40(1):16-31.Hu W S,LüB Q,Zhang W J,Mao Z G,Leng J,Guan D Y.2005.An approach to tectonic evolution and dynamics of the Songliao Basin[J].Chinese Journal of Geology,40(1):16-31(in Chinese).
黄媛,吴建平,张天中,张东宁.2008.汶川8.0级大地震及其余震序列重定位研究[J].中国科学:D辑,38(10):1242-1249.Huang Y,Wu J P,Zhang T Z,Zhang D N.2008.Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence[J].Science in China:Series D,51(2):1703-1711.
李恩泽,刘财,张良怀,曾昭发.2012.松辽盆地地震构造与地震活动相关性研究[J].地球物理学进展,27(4):1337-1349.Li E Z,Liu C,Zhang L H,Zeng Z F.2012.The correlation of structure and earthquake in Songliao Basin[J].Progress in Geophysics,27(4):1337-1349(in Chinese).
李圣强,陈棋福,赵里,朱露培,高金哲,李闽峰,刘桂平,王斌.2013.2011年5月中国东北MW5.7深震的非同寻常震源机制:区域波形反演与成因探讨[J].地球物理学报,56(9):2959-2970.Li S Q,Chen Q F,Zhao L,Zhu L P,Gao J Z,Li M F,Liu G P,Wang B.2013.Anomalous focal mechanism of the May 2011MW5.7 deep earthquake in northeastern China:Regional waveform inversion and possible mechanism[J].Chinese Journal of Geophysics,56(9):2959-2970(in Chinese).
李志田,赵成弼,郭孟习.2002.第二松花江断裂活动性剖析[J].吉林地质,21(1/2):15-19.Li Z T,Zhao C B,Guo M X.2002.Analysis of the Second Songhua River fault activities[J].Jilin Geology,21(1/2):15-19(in Chinese).
刘权锋,盛俭,卢滔,张洪艳,盘晓东.2017.扶余/松原-肇东断裂研究综述[J].防灾科技学院学报,19(3):8-16.Liu Q F,Sheng J,Lu T,Zhang H Y,Pan X D.2017.Research status of Fuyu/Songyuan-Zhaodong fault[J].Journal of Institute of Disaster Prevention,19(3):8-16(in Chinese).
罗钧,赵翠萍,周连庆.2014.川滇块体及周边区域现今震源机制和应力场特征[J].地震地质,36(2):405-421.Luo J,Zhao C P,Zhou L Q.2014.Characteristics of focal mechanisms and stress field of the Chuan-Dian rhombic block and its adjacent regions[J].Seismology and Geology,36(2):405-421(in Chinese).
罗艳,倪四道,曾祥方,郑勇,陈祺福,陈颙.2010.汶川地震余震区东北端一个余震序列的地震学研究[J].中国科学:地球科学,40(6):677-687.Luo Y,Ni S D,Zeng X F,Zheng Y,Chen Q F,Chen Y.2010.A shallow aftershock sequence in the north-eastern end of the Wenchuan earthquake aftershock zone[J].Science China Earth Sciences,53(11):1655-1664.
罗艳,倪四道,曾祥方,谢军,陈颙,龙锋.2011.一个发生在沉积盖层里的破坏性地震:2010年1月31日四川遂宁-重庆潼南地震[J].科学通报,56(2):147-152.Luo Y,Ni S D,Zeng X F,Xie J,Chen Y,Long F.2011.The M5.0 Suining-Tongnan(China)earthquake of 31 January 2010:A destructive earthquake occurring in sedimentary cover[J].Chinese Science Bulletin,56(6):521-525.
孙文斌,和跃时.2004.中国东北地区地震活动特征及其与日本海板块俯冲的关系[J].地震地质,26(1):122-132.Sun W B,He Y S.2004.The feature of seismicity in Northeast China and its relation to the subduction of the Japan Sea Plate[J].Seismology and Geology,26(1):122-132(in Chinese).
王勤彩,王中平,张金川,李君,陈章立.2015.2010年4月玉树MS7.3地震序列的断层结构[J].地球物理学报,58(6):1931-1940.Wang Q C,Wang Z P,Zhang J C,Li J,Chen Z L.2015.Fault structure of MS7.3 Yushu earthquake sequence in April,2010[J].Chinese Journal of Geophysics,58(6):1931-1940(in Chinese).
王未来,吴建平,房立华,王长在.2012.2010年玉树MS7.1地震及其余震的双差定位研究[J].中国科学:地球科学,42(7):1037-1046.Wang W L,Wu J P,Fang L H,Wang C Z.2012.Relocation of the Yushu MS7.1 earthquake and its aftershocks in 2010 from HypoDD[J].Science China Earth Sciences,56(2):182-191.
王未来,吴建平,房立华,来贵娟.2014.2014年云南鲁甸MS6.5地震序列的双差定位[J].地球物理学报,57(9):3042-3051.Wang W L,Wu J P,Fang L H,Lai G J.2014.Double difference location of the Ludian MS6.5 earthquake sequences in Yunnan Province in 2014[J].Chinese Journal of Geophysics,57(9):3042-3051(in Chinese).
吴微微,杨建思,苏金蓉,杜文康,高瑜,郑钰,田宝峰,刘莎,吴朋.2014.2013年吉林前郭-乾安震源区中强地震矩张量反演与区域孕震环境研究[J].地球物理学报,57(8):2541-2554.Wu W W,Yang J S,Su J R,Du W K,Gao Y,Zheng Y,Tian B F,Liu S,Wu P.2014.Moment inversion of moderate earthquakes and seismogenic environment in Qianguo-Qian’an source region,2013,Jilin Province[J].Chinese Journal of Geophysics,57(8):2541-2554(in Chinese).
许忠淮.2001.东亚地区现今构造应力图的编制[J].地震学报,23(5):492-501.Xu Z H.2001.A present-day tectonic stress map for eastern Asia region[J].Acta Seismologica Sinica,23(5):492-501(in Chinese).
杨宝俊,穆石敏,金旭,刘财.1996.中国满洲里-绥芬河地学断面地球物理综合研究[J].地球物理学报,39(6):772-782.Yang B J,Mu S M,Jin X,Liu C.1996.Synthesized study on the geophysics of Manzhouli-Suifenhe geoscience transect China[J].Chinese Journal of Geophysics,39(6):772-782(in Chinese).
曾祥方,罗艳,韩立波,石耀霖.2013.2013年4月20日四川芦山MS7.0地震:一个高角度逆冲地震[J].地球物理学报,56(4):1418-1424.Zeng X F,Luo Y,Han L B,Shi Y L.2013.The Lushan MS7.0 earthquake on 20 April 2013:A high-angle thrust event[J].Chinese Journal of Geophysics,56(4):1418-1424(in Chinese).
张凤鸣,张亚江,许晓艳,张天雷,张震.2007.日本海西部-中国东北深震区俯冲运动对东北地区浅源地震的动力作用[J].东北地震研究,23(1):33-39.Zhang F M,Zhang Y J,Xu X Y,Zhang T L,Zhang Z.2007.Dynamic action on the subduction movement of the west part of Japan sea-deep focus earthquake region in northeast area of China to the shallow source earthquake in northeast area[J].Seismological Research of Northeast China,23(1):33-39(in Chinese).
张慧,焦明若,刘峡.2012.太平洋板块俯冲对中国东北深浅震影响机理的数值模拟[J].地震,32(2):135-144.Zhang H,Jiao M R,Liu X.2012.Numerical simulations of the influencing mechanism of the Pacific Plate subduction to NEChina on deep and shallow earthquakes[J].Earthquake,32(2):135-144(in Chinese).
张萍,孙文福,苗春兰,高艳玲,邹向荣.2009.东北地区中强地震震源机制解分析[J].地震地磁观测研究,30(1):12-19.Zhang P,Sun W F,Miao C L,Gao Y L,Zou X R.2009.Analysis of focal mechanism solution of moderately strong earthquakes in Northeast China[J].Seismological and Geomagnetic Observation and Research,30(1):12-19(in Chinese).
郑秀芬,欧阳飚,张东宁,姚志祥,梁建宏,郑洁.2009.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑[J].地球物理学报,52(5):1412-1417.Zheng X F,Ouyang B,Zhang D N,Yao Z X,Liang J H,Zheng J.2009.Technical system construction of data backup center for China seismograph network and the data support to researches on the Wenchuan earthquake[J].Chinese Journal of Geophysics,52(5):1412-1417(in Chinese).
郑勇,马宏生,吕坚,倪四道,李迎春,韦生吉.2009.汶川地震强余震(MS≥5.6)的震源机制解及其与发震构造的关系[J].中国科学:D辑,39(4):413-426.Zheng Y,Ma H S,LüJ,Ni S D,Li Y C,Wei S J.2009.Source mechanism of strong aftershocks(MS≥5.6)of the2008-05-12 Wenchuan earthquake and the implication for seismotectonics[J].Science in China:Series D,52(6):739-753.
Artemieva I M,Mooney W D.2001.Thermal thickness and evolution of Precambrian lithosphere:A global study[J].J Geophys Res,106(B8):16387-16414.
Gephart J W,Forsyth D W.1984.An improved method for determining the regional stress tensor using earthquake focal mechanism data:Application to the San Fernando earthquake sequence[J].J Geophys Res,89(B11):9305-9320.
Gudmundssonó,Sambridge M.1998.A regionalized upper mantle(RUM)seismic model[J].J Geophys Res,103(B4):7121-7136.
Guo Z,Chen Y J,Ning J Y,Feng Y G,Grand S P,Niu F L,Kawakatsu H,Tanaka S,Obayashi M,Ni J.2015.High resolution 3-D crustal structure beneath NE China from joint inversion of ambient noise and receiver functions using NECESSArray data[J].Earth Planet Sci Lett,416:1-11.
Hardebeck J L,Michael A J.2006.Damped regional-scale stress inversions methodology and examples for southern California and the Coalinga aftershock sequence[J].J Geophys Res,111(B11):B11310.
Helmberger D V,Engen G R.1980.Modeling the long-period body waves from shallow earthquakes at regional ranges[J].Bull Seismol Soc Am,70(5):1699-1714.
Pasyanos M E,Masters T E,Laske G,Ma Z.2014.LITHO1.0:An updated crust and lithospheric model of the Earth[J].J Geophys Res,119(3):2153-2173.
Lund B,Townend J.2007.Calculating horizontal stress orientations with full or partial knowledge of the tectonic stress tensor[J].Geophys J Int,170(3):1328-1335.
Martínez-Garzón P,Kwiatek G,Sone H,Bohnhoff M,Dresen G,Hartline C.2014.Spatiotemporal changes,faulting regimes,and source parameters of induced seismicity:A case study from the Geysers geothermal field[J].J Geophys Res,119(11):8378-8396.
Michael A J.1984.Determination of stress from slip data:Faults and folds[J].J Geophys Res,89(B13):11517-11526.
Waldhauser F,Ellsworth W L.2000.A double-difference earthquake location algorithm:Method and application to the northern Hayward fault,California[J].Bull Seismol Sco Am,90(6):1353-1368.
Waldhauser F,Ellsworth W L.2002.Fault structure and mechanics of the Hayward fault,California,from double-difference earthquake locations[J].J Geophys Res,107(B3):ESE 3-1-ESE 3-15.
Wan Y G.2010.Contemporary tectonic stress field in China[J].Earthquake Science,23(4):377-386.
Zhao L S,Helmberger D V.1994.Source estimation from broad-band regional seismograms[J].Bull Seismol Soc Am,84(1):91-104.
Zhu L P,Helmberger D V.1996.Advancement in source estimation techniques using broadband regional seismograms[J].Bull Seismol Soc Am,86(5):1634-1641.
Zhu L P,Rivera L A.2002.A note on the dynamic and static displacements from a point source in multilayered media[J].Geophys J Int,148(3):619-627.
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