简介：通过文献调查、专家组访谈、实地调查等方式搜集资料,从决策部署和组织指挥、自救互救、医疗救治与卫生防疫、紧急安置等方面对玉树7.1级地震抢险救灾活动进行了综述。

简介：利用玉树、曲玛莱、杂多地震台观测到的数字震相资料，研究玉树Ms7．1级地震前后波速比时间演化特征。研究发现：3个台站平均波速比、波速比标准偏差在地震前后变化不相同，Ms4．7级前震发生时3个台站波速比都出现较明显的高值回返现象，其中玉树地震台波速比数值高达2．032。

简介：介绍了玉树7.1级地震震情跟踪过程中,数字地震观测资料的应用情况,发现数字地震资料的运用可以为震后趋势判定提供参考依据。

简介：从灾情收集、地震现场、震情监测、趋势研判、区域联动、信息发布、后勤保障、灾害评估等方面对青海省地震系统在玉树地震中的应急工作进行了概述。

简介：Ms7.1Yushu地震的seismogenic差错的coseismic表面破裂地区包括三左走的主要破裂，给300以畲獧吗？

简介：2010年4月14日青海省玉树发生MS7.1级地震,造成严重的人员伤亡和重大的经济损失。除组织现场快速震害评估和地表破裂带调查外,利用高分辨率卫星影像解译是迅速给出初步震害评估和同震地表破裂的位置和展布的最佳途径。本文通过对震前、震后高分辨率SPOT卫星影像的对比,解译出了12km长的同震地表破裂带,其在影像上主要表现为线性阴影和色彩变化。地表破裂带位置和先存的断层、老破裂带位置一致,说明青海玉树地震属于原地复发型地震。同时,解译结果也得到了来自野外实地调查结果的验证,证明了遥感解译的可信性和及时性。但解译破裂长度远小于实际破裂长度,也说明了基于2.5m分辨率的SPOT卫星影像的遥感解译存在较大的局限性。

简介：新形势下,地方地震局必须转变观念、不断加强和改进防震减灾工作内容和工作方式,才能满足社会需求。主要论述玉树7.1级地震后,海东市地震局在防震减灾工作中存在的问题和改进措施。

简介：继2008年5月12日汶川8.0级地震之后,2010年4月14日我国大陆西部的青海玉树又发生了7.1级地震,造成了巨大的生命财产损失。值此玉树地震5周年之际,对该区域地震的预测研究进行回顾,从地震前兆资料、地震大形势、构造相互作用、应力的积累与释放、周边大震的影响等方面进行了经验总结和讨论。分析认为地震中长期预测仍将是地震预报和地震短临预报的突破口,从大的背景判定危险区域,投入监测力度,进而进行小区域研究分析,在震前找到一定的前兆信息或者资料积累等仍将是未来的努力方向。

简介：Theauthorsstudiedtheseismicactivity,precursoryanomaliesandabnormalanimalbehaviorbeforetheApril14,2010MS7.1Yushuearthquake.AnalysisshowedthatanomalieswerenotrichbeforetheMS7.1Yushuearthquake,butprominentanomalieswereobserved,suchasthelongandmid-termtrendanomalycharacterizedbytheseismicquiescenceofMS6.0,MS5.0andMS4.0earthquakes,andtheanomaliesinprecursorobservationofsurfacewatertemperatureinYushuandDelinghaandelectromagneticmeasurementinPingan.Therewerealargenumberofanimalbehavioranomaliesappearingoneweekbeforetheearthquake.AnM4.7earthquakeoccurred130minutesbeforethemainshock.Inthispaper,westudiedthedynamicprocessoftheYushuearthquakepreparationusingtheearthquakefocalmechanismsolutionsontheBayanHarblockboundarysince1996.TheresultsshowthattheKalakunlunM7.1earthquakein1996,theManiM7.5earthquakeandtheYushuMS7.1earthquakehavethesamedynamicprocess.Longandmid-termtrendanomaliesmayberelatedtothedynamicsofevolutionofdifferentearthquakes.Thispaperalsodiscussestherecurrenceintervalofstrongearthquakes,foreshockidentificationandprecursorobservationoftheYushuMS7.1earthquake.

简介：利用中国数字地震台网（CDSN）的7个台站记录的2010年4月14日玉树地震的波形资料,采用功率谱方法测定相继时间间隔内较清楚地球自由振荡频谱峰的能量,并采用最小二乘拟合方法确定了相应振型的Q值。结果表明不同振型的Q值明显不同,同一振型在不同台站计算得到的Q值也有略微差异。分析认为,前者可能源于地球自由振荡振型频率和探测深度不同所致,而后者可能与地壳的横向不均匀特性有关。

简介：The2010YushuMS7.1earthquakeoccurredinGanzi-Yushufault,whichisthesouthboundaryofBayanHarblock.Inthisstudy,byusingdoubledifferencealgorithm,thelocationsofmainshock(33.13°N,96.59°E,focaldepth10.22km)andmorethan600aftershockswereobtained.ThefocalmechanismsofthemainshockandsomeaftershockswithMS>3.5wereestimatedbyjointlyusingbroadbandvelocitywaveformsfromGlobalSeismicNetwork(GSN)andQinghaiSeismicNetworkaswell.Thefocalmechanismsandrelocationshowthatthestrikeofthefaultplaneisabout125°(WNW-ESE),andthemainshockisleft-laterallystrike-slip.Theparametersofshear-wavesplittingwereobtainedatseismicstationsofYUSandL6304bysystematicanalysismethodofshear-wavesplitting(SAM)method.Basedontheparametersofshear-wavesplittingandfocalmechanism,thecharacteristicsofstressfieldinseismicsourcezonewereanalyzed.ThedirectionsofpolarizationatstationsYUSandL6304aredifferent.ItisconcludedthatafterthemainshockandtheMS6.3aftershockonApril14,thestress-fieldwaschanged.

简介：ＴｈｅｂｖａｌｕｅｓｐｅｃｔｒｕｍａｎｄηｖａｌｕｅｂｙｔｈｅｍｏｍｅｎｔｍｅｔｈｏｄＴｏｒｕＯｕｃｈｉ（大内）ＤｅｐａｒｔｍｅｎｔｏｆＥａｒｔｈＳｃｉｅｎｃｅｓ，ＦａｃｕｌｔｙｏｆＳｃｉｅｎｃｅ，ＫｏｂｅＵｎｉｖｅｒｓｉｔｙ，Ｋｏｂｅ，６５７，...

简介：ＣａｌｃｕｌａｔｉｏｎｏｆｂｖａｌｕｅａｎｄｉｔｓａｐｐｌｉｃａｔｉｏｎｉｎｅａｒｔｈｑｕａｋｅｐｒｅｄｉｃｔｉｏｎＨｕａ－ＣｈｅｎＤＵＡＮ（段华琛）；Ｃｈａｎｇ－ＱｉｎｇＦＡＮ（范长青）ａｎｄＹｕｅ－ＭｉｎＸＵ（许跃敏）（Ｓｅｉｓｍｏｌｏｇｉｃａｌ...

简介：Intheestimationofseismictendency,usingGutenberg-Richter￠sb-valueandusingHurstexponentaretwocom-monlyusedmethods.Basedonthefractalgeometryofearthquaketimeseries,wepointoutthatthesetwomethodscorrelatetoeachother.IntheperspectiveoffractionalBrownianmotion(FBM),anearthquakesequencewithb>3/4andthatwithb<3/4havedifferentdynamicproperties.

简介：本文讨论可信的历史地震资料和现代化仪器记录资料的统一使用问题。

简介：Basedonisotropiclinearporoelastictheoryandundertheundrainedcondition,wesummarizethreeequationsconnectingtheSkempton’scoefficientBwiththegroundwaterlevel.Afteranalysis,weproposeamethodtocalculatetheSkempton’scoefficientBaccordingtotherelationshipbetweenwaterlevelandtidalstrain.WiththismethodwecangetthevalueofBwithouttheearthquakeoccurrence,whichcanprovidethehighfrequencywavesforresearch.Besides,wecanalsogetthein-suitSkempton’scoefficientBwithouttheexperimentofrockphysics.Inaddition,weanalyzetheobserveddataofChangpingstationrecordedingroundwatermonitoringnetwork(abv.,GMN)beforeandaftertheWenchuanMS8.0withthismethod,andfindoutthere’saslightchangeofthevalueofBaftertheseismicwavespassedby,whichimpliesthatthepropagationofseismicwavesmayhavebroughtsomevariationstotheporoelasticmediumofthewell.

简介：Inthisstudy,weadoptanimprovedBayesianapproachbasedonfree-knotB-splinebasestostudythespatialandtemporaldistributionoftheb-value.SynthetictestsshowthattheimprovedBayesianapproachhasasuperiorperformancecomparedtotheBayesianapproachaswellasthewidelyusedmaximumlikelihoodestimation(MLE)methodinfittingtherealvariationofb-values.WethenapplytheimprovedBayesianapproachtoNorthChinaandfindthattheb-valuehasaclearrelevancetoseismicity.Temporalchangesofb-valuesarealsoinvestigatedintwospecificareasofNorthChina.Weinterpretsharpdecreasesintheb-valuesasusefulmessagesinearthquakehazardanalysis.

简介：TheeffectsofmagnituderoundingandofthepresenceofnoiseintheroundedmagnitudesontheestimationoftheGutenberg–Richterb-valueareexplored,andthewaystocorrectfortheseeffectsareproposed.Fortypicalvalues,b=1androundingintervalDM=0.1,theroundingerrorisapproximately-10-3anditcanbecorrectedtoanegligibleapproximately-10-5.Forthesametypicalvalues,theeffectofnoisecanbelarger,dependingonthecharacteristicsofthenoisedistribution;fornormallydistributednoisewithstandarddeviationr=0.1,thecorrectb-valuemaybeunderestimatedbyafactor*0.97.

简介：ＡｍｏｄｅｌｏｆｓｅｉｓｍｉｃｉｔｙｗｉｔｈｆｒａｃｔａｌｓｔｒｕｃｔｕｒｅｓａｎｄａｐｒｅｌｉｍｉｎａｒｙｄｉｓｃｕｓｓｉｏｎｏｎｔｈｅｒｅｌａｔｉｏｂｅｔｗｅｅｎＤａｎｄｂｖａｌｕｅＨａｔ－ＫｕｎＪＩＡＮＧ（蒋海昆）ａｎｄＳｈｏｕ－ＺｈｏｎｇＤＩ...

简介：ＣｕｍｕｌａｔｉｖｅｆｒｅｑｕｅｎｃｙｂｖａｌｕｅｗｉｔｈｏｕｔｕｐｐｅｒｂｏｕｎｄｍａｇｎｉｔｕｄｅａｎｄｉｔｓｒｅｇｒｅｓｓｉｏｎｄｅｔｅｒｍｉｎａｔｉｏｎＪｉａｎ－ＷｅｎＳＨＥＮ（沈建文）（ＳｅｉｓｍｏｌｏｇｉｃａｌＢｕｒｅａｕｏｆＡｎｈｕｉＰ...