简介：Becauseofitsexcellentseismicperformance,reinforcedsoilretainingwallsareincreasinglyusedincivilengineering.Althoughmanycountrieshavepublishedcorrespondingdesigncodes,thedifferencesbetweenthemarestillrelativelylarge.UsingtheFHWACodeandtheCodeforSeismicDesignofRailwayEngineering(CSDRE),stabilitycalculationsofreinforcedsoilretainingwallswerecarriedoutandthesimilaritiesanddifferencesbetweenthesetwodesigncodeswereanalyzed.Accordingtothecomparativeanalysis,thefollowingconclusionsaredrawn:theinertiaforce,theearthpressureandthetensileforceofreinforcementscalculatedfromtheCSDREarelessthanthosefromtheFHWACode,andthesafetyfactorcalculatedfromtheformerislarger.AlthoughtheM-Omethodisrecommendedtocalculatethedynamicearthpressure,theFHWACodesuggestsahigheractionpointascomparedtotheCSDRE.

简介：ThecharacteristicsofseismicgroundmotionsinsouthernChinaaredifficulttodeterminestatisticallyduetoalackofstronggroundmotiondata.Inthisstudy,astochasticfinite-faultgroundmotionmodelwasadoptedtosimulatetheseismicgroundmotionsatbedrockforsouthernChina,basedonparametersderivedfromsmallandmediumearthquakesthathaveoccurredintheregion.Fromthese,theresponsespectrawasestimated.Asetofgroundmotionattenuationrelationshipswasthendevelopedbasedonsimulatedpeakgroundmotionsandresponsespectralparametersthroughregression,whichwouldbeapplicableforuseinengineeringpractice.Throughcomparisons,itwasdemonstratedthattheproposedgroundmotionrelationshipsaregenerallyconsistentwiththoseobtainedfromotherreportedgroundmotionattenuationmodelsforsouthernChina.

简介：At19:33p.monSeptember27,2003,anearthquakewithM7.9occurredintheRussiaMongolia-ChinaboundaryRegion.ItwasstronglyfeltintheAltayregionofXinjiang.Thelossescausedbytheearthquakewas76millionyuan(RMB).Someinformationabouttheearthquakewasoutlined,includingbasicparameters,focalmechanism,evaluationofearthquakedisasterlossesandsoon.Thesatelliteremotesensinginformationworkedinitialanalysisfordeformationofgroundandfailurephenomenon.

简介：ThenorthernLiulengshanpiedmontfaultislocatedalongthesouthernmarginoftheYangyuanbasinandrepresentsadip-slipnormalfault,generallyNEE-trendingandNNW-dipping.LandformsoffsetbythefaultarefairlydevelopedandwellpreservedintheDushanpuareaofYangyuanCounty,HebeiProvince.TwotrencheswereexcavatedinfrontofascarpofthenorthernLiulengshanpiedmontfaultatDushanpuandtwopaleoseismiceventswererevealedinthetrenches,fromwhichseveralsampleswerecollectedfordating.ThesamplesweredatedusingtheIRSLdatingtechnique.Thepreliminaryresultshowsthepossibleagesofthetwopaleoseismicevents.

简介：Studyofgeothermalfielddata,terrestrialheatflowvalues,andothergeophysicaldatafromtheXingtai-ShuluareaofHebeiProvincemadeusmoreunderstandingofthedistributionofgeothermalfieldsanddeepstructuresandtheirinterrelation.Thestudyillustratesthatthegeothermalfieldhasanapparentlateralinhomogeneityandisevidentlycorrelatedbythestructureofthecrustanduppermantleinthearea.Therelationofthegeothermalfielddistributiontothestructureindicatesthatincomparisonwiththedepressionzone,theupliftzonehasahigherheatflowvalueandalargergeothermalgradient.Theanalysisoftherelationbetweendistributionofearthquakeepicentersandgeothermalfieldandmathematicalsimulationofthermalstressintheareasuggeststhatthermalstressplaysanimportantroleintheprocessofearthquakegeneration.

简介：MomenttensorsolutionswereretrievedfortheearthquakeswarmthatoccurredduringNovemberandDecember2010intheBoshanminingarea,ShandongProvince,China.Theresultsshowedthatthedouble-couplecomponentsinthesourcemechanismswerehigheratthebeginningoftheswarmandconsistedmainlyofshearfaultingcontrolledbytectonicstress.Thesubsequenteventshadsignificantnon-double-couplecomponents,indicatingtensilefaulting.Thedouble-couplecomponentspredominatelypresentedasnormalfaultingandthePaxeswereorientatedalmostvertically.Theslipvectorsoftheswarmeventswererelativelystable.Withreferencetothetectonicfeaturesneartheepicenter,weconcludedthattheswarmwasaresultofsubordinatefaultmotionrelatedtotheWangmuMountainfaultandthathigh-pressureporefluidsplayedacrucialroleintheactivityoftheearthquakeswarm.

简介：Basedonthecasestudiesandstatisticalanalysisofearthquake-relatedionosphericdisturbancesmainlyfromDEMETERsatellite,ground-basedGPSandionosoundingdata,thispapersummarizesthestatisticalcharacteristicsofearthquake-relatedionosphericdisturbances,includingelectromagneticemissions,plasmaperturbationsandvariationofenergeticparticleflux.AccordingtothemainresultsdonebyChinesescientists,fusingwiththeexistedstudyfromglobalresearches,seismo-ionosphericdisturbancesusuallyoccurredafewdaysorhoursbeforeearthquakeoccurrence.Parallelingtothesecasestudies,lithosphere-atmosphere-ionosphere(LAI)couplingmechanismsarecheckedandoptimized.Athermo-electricmodelwasproposedtoexplaintheseismo-electromagneticeffectsbeforeearthquakes.Apropagationmodelwasputforwardtoexplaintheelectromagneticwavesintotheionosphere.Accordingtotherequirementofearthquakepredictionresearch,Chinaseismo-electromagneticsatellite,thefirstspace-basedplatformofChineseearthquakestereoscopicobservationsystem,isproposedandplannedtolaunchatabouttheendof2014.ItfocusesoncheckingtheLAImodelanddistinguishingearthquake-relatedionosphericdisturbance.ThepreliminarydesignforthesatellitewilladoptCAST-2000platformwitheightpayloadsonboard.Itisbelievedthatthesatellitewillworktogetherwiththegroundmonitoringnetworktoimprovethecapabilitytocaptureseismo-electromagneticinformation,whichisbeneficialforearthquakemonitoringandpredictionresearches.

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简介：通过对西宁市区28个街道办事处的各类房屋建筑面积的调查了解，进行了对西宁市区的房屋建筑的静态震害预测，当西宁及周边地区发生破坏性地震、波及西宁市区时进行快速评（盲）估工作提供较为科学的定量的参考数据。

简介：信息技术的采用大大提高了震害预测的精度和震灾快速评估能力。城市震害预测工作在地理信息系统和计算机模拟技术支持下,能有效对震灾的发生及时获取各种基础数据进行综合分析,并对震害造成的损失和社会影响进行科学估算。利用数字城市为我们提供的数据共享平台和技术系统,帮助政府快速了解震情、灾情、提出对策。同时,依据震害预测研究成果,结合数字城市、数字福建可为政府及有关部门了解防灾薄弱环节,采取减灾措施,制定城市减轻灾害的长远规划,提高城市抗御地震灾害的能力

简介：ThispaperreportstheinternalstructuresoftheBeichuanfaultzoneofLongmenshanfaultsystemthatcausedthe2008Wenchuanearthquake,atanoutcropinHongkou,Sichuanprovince,China.PresentworkisapartofcomprehensiveprojectofInstituteofGeology,ChinaEarthquakeAdministration,tryingtounderstanddeformationprocessesinLongmenshanfaultzonesandeventuallytoreproduceWenchuanearthquakebymodelingbasedonmeasuredmechanicalandtransportproperties.Outcropstudiescouldbeintegratedwiththoseperformedonsamplesrecoveredfromfaultzonedrilling,duringtheWenchuanEarthquakeFaultScientificDrilling(WFSD)Project,tounderstandalong-faultanddepthvariationoffaultzoneproperties.Thehangingwallsideofthefaultzoneconsistsofweakly-foliated,clayeyfaultgougeofabout1minwidthandofseveralfaultbrecciazonesof30-40mintotalwidth.Wecouldnotfindanypseudotachyliteatthisoutcrop.DisplacementduringtheWenchuanearthquakeishighlylocalizedwithinthefaultgougelayeralongnarrowerslipping-zonesofabout10to20mminwidth.Thisisanimportantconstraintforanalyzingthermalpressurization,animportantdynamicweakeningmechanismoffaults.Overlappingpatternsofstriationsonslickensidesurfacesuggestthatseismicslipatagiventimeoccurredinevennarrowerzoneofafewtoseveralmillimeters,sothatlocalizationofdeformationmusthaveoccurredwithinaslippingzoneduringcoseismicfaultmotion.Faultbrecciazonesareboundedbythinblackgougelayerscontainingamorphouscarbon.Faultgougecontainsilliteandchloriteminerals,butnotsmectite.Clayeyfaultgougenexttocoseismicslippingzonealsocontainsamorphouscarbonandsmallamountsofgraphite.ThestructuralobservationsandmineralogicaldataobtainedfromoutcropexposuresofthefaultzoneoftheWenchuanearthquakecanbecomparedwiththoseobtainedfromtheWFSD-1andWFSD-2boreholes,whichhavebeendrilledveryclosetotheHongkououtcrop.Thepresenceofcarbonandgr

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简介：Becauseseismicactivitywithinmid-continentsisusuallymuchlowerthanthatalongplateboundaryzones,evensmallearthquakescancausewidespreadconcerns,especiallywhentheseeventsoccurinthesourceregionsofpreviouslargeearthquakes.However,thesesmallearthquakesmaybejustaftershocksthatcontinuefordecadesorevenlonger.TherecentseismicityintheTangshanregioninNorthChinaislikelyaftershocksofthe1976GreatTangshanearthquake.ThecurrentearthquakesequenceintheNewMadridseismiczoneincentralUnitedStates,whichincludesaclusterofM*7.0eventsin1811–1812andanumberofsimilareventsinthepastmillennium,isbelievedtoresultfromrecentfaultreactivationthatreleasespre-storedstrainenergyinthecrust.Ifso,thisearthquakesequenceissimilartoaftershocksinthattheratesofenergyreleaseshoulddecaywithtimeandthesequenceofearthquakeswilleventuallyend.WeusesimplephysicalanalysisandnumericalsimulationstoshowthatthecurrentsequenceoflargeearthquakesintheNewMadridfaultzoneislikelyendingorhasended.Recognizingthatmid-continentalearthquakeshavelongaftershocksequencesandcomplexspatiotemporaloccurrencesarecriticaltoimprovehazardassessments.

简介：OnApril25,2015,aM_S8.1earthquakeoccurredinNepal.IntheTibetareaofChina,thisearthquakecausedheavycasualtiesanddamagetohousing,roads,communications,otherlifelineengineering,waterconservancyandotherinfrastructure.Thispaperintroducesthebasicsituationoftheearthquake,andbasedontheinvestigationandassessmentofseismicintensity,thedamageofthedisasterareaisanalyzed,andbuildingtypesanddamagetothelifelinesystemsandvariousindustriesaregiven.Throughtheanalysisofthecharacteristicsoftheearthquakedisaster,thispaperpointsouttheexistingproblemsinseismicfortification,andfinallyputsforwardproposalsforthepreventionandcontrolofearthquakegeologicaldisasters,scientificplanningfortherestorationandreconstruction,strengtheningearthquakepreventionanddisasterreductionpropaganda,improvingtheawarenessofearthquakepreparednessintheagriculturalandpastoralareas,strengtheningtheguidanceandsupervisionofhousingconstructioninruralareastoreducethecasualtiesandlosses,andpromotingtheharmoniousdevelopmentofeconomyinTibet.

简介：根据国内外已发生水库诱发地震震例资料,结合金钟水库库区的具体情况,应用概率预测法、综合影响参数预测法、两级模糊评判法、古登堡——里克特公式外推预测法、历史地震最高震级预测法等方法对金钟水库可能诱发的最大震级进行预测研究。

简介：Ontheconditionthatthevelocityratioofcompressivewavetoshearwaveisstableduringthepropagatingprocessofseismicwave,thispaperdevelopsanestimationmethodformediumqualityfactorbasedonsinglestation'straveltimedifferencebetweendirectSandPwavesandthefirstperiodsignalofdirectPwave.8774highSNRwavedataaltogetherrecordedby75stationsareanalyzed.Theresultsshowthat:(1)underthenormalregionalstressfield,thequalityfactorsQmSPinthestabletectonicareaarehigherthanthatintheactivetectonicareaaroundtheWeifang-JiashansectionanditssurroundingareaintheTanlufaultzone;(2)intheJuxian-Tanchengsectiontheseismicwaveattenuationisrelativelyquick,andthemediaisrelativelybroken,suggestingnotectonicstressaccumulation;(3)theXinyi-Sihongsectioniscurrentlylockingandinaccumulatingelasticstrainenergystage,whichhasthedeepenvironmentandconditionsofstrongearthquakegenerationsimilartothoseofthe1668M8.5Tanchengstrongearthquake.

简介：ＰｒｅｌｉｍｉｎａｒｙｒｅｓｕｌｔｓｏｎｋｉｎｅｍａｔｉｃｍｏｄｅｌｏｆｔｅｃｔｏｎｉｃｂｌｏｃｋｓｄｅｒｉｖｅｄｆｒｏｍｈｉｇｈｐｒｅｃｉｓｉｏｎＧＰＳｏｂｓｅｒｖａｔｉｏｎｓｉｎＳｏｕｔｈｗｅｓｔＣｈｉｎａＬＩＲＥＮＨＵＡＮＧ１）（黄立人）...

简介：Buisomg126earthquakefocalmechanismsolutions(Ms≥4.7)duringtheperiodof1963-1998,moderntectonicstressfieldinNorthChinaisinvertedbymeansofthestepbystepconv-ergence.Theinversionresultsindicatethatthetectonicstressfieldintheresearchregionisclearlyvariationalinspaceandtime:(1)Themiddlingprincipalstressaxisó2isbasicallyver-tical.Themaximumandminimumprincipalstressaxesó1andó2arenearlyhorizontal,buttheazimuthsofó1andó3areinconsistentindifferentdistrictsandperiods.(2)BeforetheTangshanearthquakein1976,thethreeprincipalstressaxesareuniform.Theazimuthofmaximumprincipalstressaxisó1is68°(strikinginaNEE-SWWdirection).(3)AftertheTangshanearthquake,themaximumprincipalstressaxisó1andminimumprincipalstressaxisó3havevariationsindifferentdistricts.InthenorthernareaofNorthChinaandontheeasternsideoftheTancheng-Lujiangfaultzone,themaximumprincipalstressaxisó1isalsostrikinginaNEE-SWWdirection.Itsazimuthis68°.ItistheasmeasthatbeforetheTangshanearth-quake.InthesouthernareaofNorthChina,themaximumprincipalstressaxisó1isstrikinginaE-Wdirectionanditsazimuthis87°.

简介：Ｃｒａｃｋ－ｉｎｄｕｃｅｄａｎｉｓｏｔｒｏｐｙｉｎｔｈｅｃｒｕｓｔｆｒｏｍｓｈｅａｒｗａｖｅｓｐｌｉｔｔｉｎｇｏｂｓｅｒｖｅｄｉｎＴａｎｇｓｈａｎｒｅｇｉｏｎ，ＮｏｒｔｈＣｈｉｎａＹｕａｎＧＡＯ（高原）Ｓｉ－ＨｕａＺＨＥＮＧ；（郑斯华）ａｎｄＹｏｎｇ...

简介：Onthebasisoflocatingbythegeochemicalprospecting,shallowseismicsounding,drilling,geologicalprofiling,andneogeochronologicaldating,wefirstfoundoutthedislocationamountalongtheLiaocheng-LankaoburiedfaultsincetheQuaternaryandtheageofitslatestactivityphaseanddeterminedthattheupperbreakpointbythefaultdislocationreaches20mbelowthesurface.ThelatestactivityphasewasintheearlyHoloceneandthefaultisashallow-buriedactivefault.Anaveragedislocationratealongthefaultis0.12mm/asincetheQuaternary.Thus,itisaburiedactivefaultwithintermediatetostrongmovementstrengthintheeasternChina.