2011年日本东北地区太平洋近海地震对亚洲板块及韩国大地控制网的影响分析
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
本研究分析了2011年3月11日发生的Mw9.0日本东北地区太平洋近海地震对亚洲地区和韩国国内GPS卫星常年跟踪站的位移影响.为此,利用了日本东北地区太平洋近海地震发生前后两周(2011年3月4日到3月18日)的GPS站点数据,包括震中附近地区(韩国,中国,中国台湾地区,日本和俄罗斯)55个GPS卫星常年跟踪站和284个IGS全球跟踪站,并采用GAMIT/GLOBK软件进行处理和平差,估算出所有GPS站点的同震形变.结果显示,日本东北地区太平洋近海地震引起的同震形变影响在亚洲地区比较明显,包括日本和附近国家,距离震中2702km的中国武汉(WUHN)站也观测到同震形变.为精确分析日本东北地区太平洋近海地震对韩国国家大地控制网的影响,通过GAMIT/GLOBK软件计算出韩国GPS卫星常年跟踪站之间的基线长度变形,并分析出弹性变形量.结果表明:大部分GPS站点均向震中方向膨胀,且向震中的垂直方向收缩.由日本东北地区太平洋近海地震导致的最大剪应变达到韩国国家大地控制网年均变形率的约7倍,对韩国的地壳产生14.5~57.7mm的水平位移,并导致韩国国家大地控制网产生弹性变形.因此,在不及时更新维护韩国国家大地控制网的情况下,GPS测量成果将会发生最大20mm的位置误差.
In this study,we analyzed the effects of seismic displacements due to the megathrust earthquake occurred near Tohoku-Oki area on 11 Mar.2011 with Mw9.0 magnitude in the context of evaluation of position change by the earthquake on the Asian and Korean GPS permanent stations.For this,two weeks GPS data observed around the event of Tohoku-Oki earthquake(4 Mar—18 Mar.2011) were obtained from 55 GPS permanent stations in the vicinity of epicenter(Korea,Japan,Russia,China and Taiwan) and 284 IGS global stations.All available GPS data were processed and adjusted by GAMIT/GLOBK software to estimate the co-seismic horizontal displacements at each station.As the results of GPS analysis,the co-seismic displacements by Tohoku-Oki earthquake were clearly revealed in the GPS stations of Asian region,Japan and its neighboring countries,and even the change of horizontal position of GPS station(WUHN in China) which was about 2702 km away from the epicenter.Also,we performed the elastic deformation analysis using the deformation lengths of baselines between Korean GPS stations estimated from GAMIT/GLOBK analysis,in order to analyze the effects of Tohoku-Oki earthquake more precisely on the Korea geodetic network.Most GPS baselines of Korean geodetic network expanded in the direction of epicenter,whereas those perpendiculars to the direction of epicenter contracted.The size of maximum shear strain rate calculated during the event of Tohoku-Oki earthquake is 7 times greater than annual result of the Korean geodetic network.In conclusion,it was found that the Tohoku-Oki earthquake had resulted in the horizontal displacements,ranging from 57.7 mm to 14.5 mm in Korea.So,these irregular displacements caused the elastic deformations in Korean geodetic network and may cause a maximum error of 20 mm in GPS geodetic positioning results without updating the Korean geodetic network.
引文
[1]Nettles M,Ekstrm G,Koss H C.Centroid-moment-tensoranalysis of the 2011 Tohoku earthquake and its largerforeshocks and aftershocks.Earth Planets Space,2011,99:1-9.
    [2]Vigny C,Simons W J F,Abu S,et al.Insight into the 2004Sumatra-Andaman earthquake from GPS measurements insoutheast Asia.Nature,2005,436(7048):201-206.
    [3]Johnson K M,Hsu Y J,Segall P,et al.Fault geometry andslip distribution of the 1999 Chi-Chi,Taiwan earthquakeimaged from inversion of GPS data.Geophys.Res.Lett.,2001,28(11):2285-2288.
    [4]Yu S B,Kuo L C,Hsu Y J,et al.Preseismic deformationand coseismic displacements associated with the 1999 Chi-Chi,Taiwan earthquake.Bull.Seismol.Soc.Am.,2001,91(5):995-1012.
    [5]Satirapod C,Simons W J F,Promthong C.Monitoringdeformation of Thai Geodetic Network due to the 2004Sumatra-Andaman and 2005 Nias Earthquakes by GPS.J.Surv.Eng.,2008,134(3):83-88.
    [6]戴黎明,李三忠,陶春辉等.俯冲带耦合作用对苏门答腊地区应变场影响的三维数值模拟.地球物理学报,2010,53(8):1837-1851.Dai L M,Li S Z,Tao C H,et al.3Dnumerical modeling ofstrain field in Sumatra area influenced by the coupling effectof subduction zone.Chinese J.Geophys.(in Chinese),2010,53(8):1837-1851.
    [7]邵志刚,武艳强,江在森等.基于GPS观测分析日本9.0级地震同震位错与近场形变特征.地球物理学报,2011,54(9):2243-2249.Shao Z G,Wu Y Q,Jiang Z S,et al.The analysis ofcoseismic slip and near-field deformation about Japanese 9.0earthquake based on the GPS observation.Chinese J.Geophys.(in Chinese),2011,54(9):2243-2249.
    [8]易桂喜,龙锋,张致伟.汶川Ms8.0地震余震震源机制时空分布特征.地球物理学报,2012,55(4):1213-1227.Yi G X,Long F,Zhang Z W.Spatial and temporal variationof focal mechanisms for aftershocks of the 2008 Ms8.0Wenchuan earthquake.Chinese J.Geophys.(in Chinese),2012,55(4):1213-1227.
    [9]Subaraya C,Chlieh M,Prawirodirdjo L,et al.Plate-boundary deformation associated with the great Sumatra-Andaman earthquake.Nature,2006,440(7080):46-51.
    [10]Ozawa S,Nishimura T,Suito H,et al.Coseismic andpostseismic slip of the 2011 magnitude-9 Tohoku-Okiearthquake.Nature,2011,475(7356):373-376.
    [11]The GEONET Group,Geographical Survey Institute.GEONET(GPS Earth Observation Network System)and itsprospect.Journal of the Geodetic Society of Japan(inJapanese),2004,50(2):53-65.
    [12]国土地理院.平成23年(2011年)東北地方太平洋沖地震.により測量成果の公表を停止,http:∥www.gsi.go.jp/sokuchikijun/sokuchikijun60007.html,2011[2011-03-14].Geospatial Information Authority of Japan.Stop thepublication of survey results by the Pacific Ocean earthquakeoff the coast of the Tohoku region Heisei 23(2011),http://www.gsi.go.jp/sokuchikijun/sokuchikijun60007.html[2011-03-14].
    [13]Nikolaidis R.Observation of geodetic and seismic deformationwith the Global Positioning System[Ph.D.thesis].San Diego:University of California,2002.
    [14]King R W,Bock Y.Documentation for the GAMIT GPSanalysis software,release 10.3.Cambridge:MassachusettsInstitute of Technology,2006.
    [15]Herring T A.GLOBK Global Kalman Filter VLBI and GPSAnalysis Program,Version 10.1.Cambridge:MassachusettsInstitute of Technology,2005.
    [16]Lee Y J,Lee H K,Jeong K H,et al.Korean geodetic datum(KGD2002):nationwide GPS network definition.∥ProceedingsFIG Working Week 2008-Integrating Generations.Stockholm,Sweden,2008.
    [17]Jung K H,Ryu S H,Lee Y J,et al.Nationwide geodeticadjustment of integrated GPS networks in Korea.∥FIGCongress 2010,Facing the Challenges-Building the Capacity.Sydney,Australia,2010:11-16.
    [18]Prescott W H,Savage J C,Kinoshita W T.Strainaccumulation rates in the western United States between 1970and 1978.J.Geophys.Res.,1979,84(B10):5423-5435.
    [19]Cho J M.Crustal Deformation Analysis from Permanent GPSStations in the Korean Peninsula[Ph.D.thesis].Suwon,Korea:Sungkyunkwan University,2006.
    [20]Kutoglu H S,Mekik C,Akcin H.A comparison of two wellknown models for 7-parameter transformation.The AustralianSurveyor,2002,47(1):24-30.

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