简介：Ｅｐｉｃｅｎｔｒａｌ　ｄｉｓｔｒｉｂｕｔｉｏｎ　ｉｎ　１９９４Ｐｅｉ－ＳｈａｎＣＨＥＮ（陈培善）（ＩｎｓｔｉｔｕｔｅｏｆＧｅｏｐｈｙｓｉｃｓ，ＳｔａｔｅＳｅｉｓｍｏｌｏｇｉｃａｌＢｕｒｅａｕ，Ｂｅｉｊｉｎｇ１０００８１，Ｃｈｉｎａ）Ｐｅｉ－ＳｈａｎＣ...

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简介：Slipdistributionofthe1979ImperialValley,1989LomaPrieta,1992Landers,1994Northridge,and1995Kobeearthquakeshowsapiece-wiseGutenberg-Richter'slaw.Forsmallslips,theb-valueisnearto1;whileforlargeslips,theb-valueislargerthan1.

简介：Thisarticlepresentsanapplicationofaproceduretomodifytheintensitydistributionbyassessingthereliability.Therearetwopotentialpossibilitiesthatmayinfluencetheintensitydistribution:(1)Fortheinterpolationerror,wegenerateameasuredgridacrossthecalculationregion.Whenthepointtostationspacingis\5km,weconsidertheresultsprecise;however,somepointshavelessprecisionbecausethesearefartherfromthecorrespondingstations.Whenthespacingisbetween5and50km,weconsidertheresultsimpreciseanddefineareliabilityfactorthatcorrelateswiththedistance.(2)Somerecordsmayhaveerrorsthatresultfromlocalsiteconditions,equipmentproblems,orsomedisturbancesuchaslightningstroke,whichwillleadtosomegridpointshavinganincorrectintensity.Weregresstheattenuationrelationforsiteswithabnormalintensitiesandconsidertheresultstobeaccuratewhenthestandarddeviation(STD)is\randinaccuratewhentheSTDis[2r.WethendefineareliabilityfactortocorrelatewithSTDbetweenrand2r,suchthattheintensitydistributionisinaccordwithbothwavepropagationtheoryandtheinvestigationintensity.

简介：ＧｅｏｇｒａｐｈｉｃａｌｄｉｓｔｒｉｂｕｔｉｏｎｏｆｈｙｐｏｃｅｎｔｒａｌｄｅｐｔｈｓｏｆＣｈｉｎｅｓｅｅａｒｔｈｑｕａｋｅｓＸＩＮＧ－ＢＥＩＤＵＡＮ（段星北）ＩｎｓｔｉｔｕｔｅｏｆＧｅｏｐｈｙｓｉｃａｌ，ＳｔａｔｅＳｅｉｓｍｏｌｏｇｉｃａｌＢｕｒ...

简介：SeveralfactorsareselectedtoreflectthetemporalandspatialfeaturesofseismicityinSouthwestChina.Themeasurementsofthefactorsarealltakenfromthestatisticalrelationbetweenthefactorsandactualearthquakes,andmakethefactorspossessacertainprobabilisticpredictionmeaningandthebaseformutualcontrast.Theeffectsofpredictionofpartofthefactorshavebeenevaluatedandusedtocorrectthefactors.Threesetsofseismicspatialdistributionfunctionshavebeencalculatedbyusingthreedifferentmethodsanddiscussedindetail.

简介：Asoneofthemostimportanturbanlifelinesystems,awaterdistributionsystemcanbedamagedunderastrongearthquake,andthedamagecannoteasilybelocated,especiallyimmediatelyaftertheevent.Thisoftencausestremendousdifficultiestopost-earthquakeemergencyresponseandrecoveryactivities.Thispaperproposesamethodologytolocateseismicdamagetoawaterdistributionsystembymonitoringwatcrheadonlineatsomenodesinthewaterdistributionsystem.Anartificialneuralnetwork-basedinverseanalysismethodisdevelopedtoestimatethewaterheadvariationsatallnodesthatarenotmonitoredbasedonthewaterheadvariationsatthenodesthataremonitored.Themethodologyprovidesaquick,effective,andpracticalwaytolocateseismicdamagetoawaterdistributionsystem.

简介：Inthispaper,thefocusdepthdistributionofearthquakeswitheachmagnitudehasbeenanalyzed.Statisticdatashowthatthelowermagnitudeis,thewiderfocusdepthdistributes.Withlargermagnitude,thefocustendstobeconcentratedinupperormiddlecrustallayers.Weanalyzedthecauseoffocusdepthdistributionandexplainedtheprecursormechanismofsmallandmoderateearthquakeswithoccurringconditionandcharacteristicsofstrongearthquakes.Theresultsofthispapermaybeappliedtodeterminerisksitesofstrongearthquakes.

简介：Byanalyzinghigher-accuracylocationdataoftheTangshanearthquakesequence,acleardistributionpatternofthreeaftershockbeltsintheNE,NWW,andNWdirectionsofhasbeenobtained.TheanalysisrevealsthreeruptureplanesofstrongeventsofMS7.8,MS7.1andMS6.9inthesequence.Itindicatesthatthecomplexpatterniscloselyrelatedtotheearthquakesource,andtheNE-,NWW-andNW-trendingregionalfaultzones,whichhavebeenrevealedbytheresearchofthepre-seismicityanomaly.Insummary,thesourceislocatedinthejunctionofthethreefaultzones,andtheruptureplanesofthethreestrongeventslocatedinthesourcecanberegardedasthelockedsegmentsonthethreefaultzones.Onthesegrounds,thepaperexplainsthecomplexityofthesourceandepicentraldistributionofaftershocks.

简介：Itisproposedthatsomepossiblemacroseismicepicenterscanbedeterminedquicklyfromtherelationshipthatthemicroseismicepicenterslocatedbyinstrumentsbearwithfaults.Basedontheseso-calledmacroseismicepicenters,wecanmakefastseismichazardestimationafterashockbyuseoftheempiricaldistributionmodelofseismicintensity.Incomparisonwiththemethodthatusesthemicroseismicepicentersdirectly,thisapproachcanincreasetheprecisionoffastseismichazardestimation.Statisticalanalysisof133mainearthquakesinChinawasmade.Theresultshowsthatthedeviationdistancebetweenthemicroseismicepicenterandmacroseismicepicenterfallswithintherangeof35kmfor88%earthquakesofthetotalandwithintherangeof35to75kmfortheremainingones.Then,wecantaketheareathathasthemicroseismicepicenterasitscenterandis35kminradiusastheareaforemphaticanalysis,andtaketheareawithin75kmaroundthemicroseismicepicenterastheareaforgeneralanalysis.Therelationbetweenthe66earthquakecasesontheN-SSeismicBeltinChinaandthespatialdistributioncharacteristicsoffaultsandtheresultsoffocalmechanismsolutionwereanalyzedindetail.Weknowfromtheanalysisthattheerrorofinstrumentalepicenterdeterminationisnottheonlyfactorthatgiveseffectstothedeviationofthemacroseismicepicenter.Inadditiontoit,thefaultsize,faultdistribution,faultactivity,faultintersectiontypes,earthquakemagnitude,etc.arealsomainaffectingfactors.Bysortingout,processingandanalyzingtheseaffectingfactors,theprincipleandproceduresforquicklydeterminingthepossiblepositionofthemacroseismicepicenterweresetup.Takingtheseasabasisandestablishinganationwidedatabaseoffaultsthatcontainsrelevantfactors,itispossibletoapplythismethodinpracticalfastestimationofseismichazard.

简介：在2010Yushu地震以后的二个小时，摇晃的紧张分发用基于地点效果的ShakeMap快速的产生系统被获得，由作者发展了，它集成原因的差错的构造设置，罢工和规模的信息，在西方的中国的焦点的机制solutions.fault破裂进程和变细关系，以及本地地点effects.The结果如下：摇紧张分发的主要的轴被指导NW-SE，平行到Yushu差错；meizoseismal区域到达紧张并且盖住300km2；紧张区域主要沿着原因的差错在区域40km东南和震中的15km西北被散布；由于本地土壤条件，有基岩上的紧张的区域的西北的部分看紧张是否从基岩变换成土壤；有紧张的区域，，分别地测量3,000km2,8,000km2，和24,000km2。

简介：AccordingtotierecordsofseismicstationnetworksofChina’scontinentandKoreaPeninsulaandthehistoricaldata,thecompleteseismicitypatternwasobtainedforthefirsttime.Theseismiczoningwasconductedbymeansoftheclusteranalysismethod.Themap’sspatialdistributionofseismicityfrom1960to1994showsthattherearethreestrongseismiczones:thefirstonestrikesintheNEdirection,fromtheJiangsuplaininChinatothecentralKoreanPeninsula;thesecondstrikesintheNWdirection,fromtheBohaiSea,ChinatothesouthernKoreanPeninsula;thethirdstrikesintheNWdirection,fromthewesternLiaoningProvincetoPyongyang.Mostofearthquakesarelocatedalongthesethreezones,theseismicintensityislowerthanthatinthemainland,andexhibitedthefeatureoffracturedcrustofamarginalseabasin.

简介：ThedistributionoftheintensityoftheMojiangMS5.9earthquakeinYunnanProvinceisexpounded,andthedamagecharacteristicsofbuildingsandthedamageratioandseismicdamageindexofvariousbuildingstructuresineachintensityareaarecomparedwiththoseofTheChineseSeismicIntensityScale.Themainbasisandmethodofseismicintensityassessmentarediscussedinthispaper.Itisconcludedthat:①Theseismicintensityshouldbebasedontheearthquakedamageofthehousingstructure,whichtakesupahighratiointheseismicintensityassessment.Itisrecommendedthatseismicintensityisestimatedbycalculatingtheaverageseismicdamageindex.②ThehighestintensityoftheMojiangMS5.9earthquakeisVIIIdegrees,withthelongaxistrendinginthenorth-westdirection.TheareaaboveVIIdegreesis5,180km^2.③TheintensitydistributionoftheMojiangMS5.9earthquakemeetsthenationalstandardandthedistributionlawofseismicintensityinYunnan.

简介：IntroductionThestudiesofseismicsourcephysicsandruptureprocessshowthatthepreparationandgenerationofanearthquakeanditsmagnitudeisrelatedtothegeologicalconditionsandthemediumpropertiesatthesourcetectonicpaFtand,atthesametime,directlytothestrengthofthese...

简介：Basedontheloadmodelofauniformisotropicsemi-infiniteelasticmedium,wededucedacalculationofverticaldisplacementandtiltandproposedamethodofcalculationofverticaldisplacementsandtiltscausedbyirregularloadonthegroundorundergroundatacertainpointwithtwo-dimensionalandthree-dimensionalshapes.Wecomparedthedifferencebetweenthesimplifiedmodelandtheirregularmodel.Finally,theverticaldisplacementsneartheirregularloadandthedistributionofhorizontaltiltarepresented.Theresultsshowthat,comparedwiththepointsimplifiedmodel,theirregularloadmodelhascertainadvantagesfordescribingthenearfield.Theestablishmentofatwodimensionalirregularloadmodelcanhelpwiththecalculationofthemodalvectorsuperpositionafterloadscattering.Thethree-dimensionalirregularloadmodelcanredistributeloadthroughdifferentweightsgiventothescatteredpointsaftertheloadscattering,andthenobtaindisplacementwiththevectorcalculationmethod.Theresultsofvectorsuperpositioncalculationfromthescatteredirregularloadbothintwo-dimensionsandthree-dimensionsareallconvergentobviouslyasgridsbecomedenser,anditisshownthatthecalculationmethodiscorrectandfeasible.

简介：Recentstudiesonassessmentofaverylowannualprobabilityofexceeding(APE)groundmotions,10-4orless,havehighlightedtheimportanceoftheupperboundofgroundmotionswhenverylowprobabilityresultsareacquired.Thetruncationleveladoptedinprobabilisticseismichazardanalysis(PSHA)shouldbedeterminedbyanaleatoryuncertaintymodel(i.e.,distributionmodel)ofgroundmotionsandthepossiblemaximumandminimumgroundmotionvaluesofaspecificearthquake.However,atthepresenttime,itisimpossibletoestablishtheupperboundmodelforgroundmotionsbasedonthesourcecharacteristicsand/orgroundmotionpropagation.McGuiresuggestedatruncationlevelbefixedatanumberof=6,orthedistributionofresidualsbetruncatedinsuchamannerthatsiteintensitycannotbegreaterthantheepicenterintensity.ThisstudyaimstofindareasonableandfeasibletruncationleveltobeusedinPSHAwhenthephysicalmechanismisnotavailabletofindtheextremegroundmotion.AmathematicalanalysisoftheinfluenceofthetruncationlevelonPSHA,casestudiesofsitesindifferentseismotectonicsettings,andadistributionanalysisofgroundmotionresidualsareconductedinthisstudy.Itisconcludedthat=4istheminimumacceptablevalueforengineeringapplicationsforAPEswithin0.002to10-4,andforlowAPEs,suchas10-5and10-6,thevalueofshouldbenolessthan5inmostregionsofChina.

简介：INTRODUCTIONItiscommonknowledgethatthedevelopmentandoccurrenceofanearthquakeisaverycomplicatedgeophysicalprocess.Anearthquakeiscausedbythelocalfailureoftheearthcrustmedium,andearthquakesaredistributedinhomogeneouslyinspace.Seismicactivities,however,arearealreflectionoftheinteractionofthefaults,whichprovidesussomeinformationconcerningtheearthcrustmediumandmayhelpuspredicttheearthquake.Therefore,thestudyoftheseismicitypatterncanbecomeameansofearthquakeprediction.Inordertoreflectdirectlythespacialdistributionofseismicactivities,thesketchofepicentraldistributionhasbeenwidetyusedinthestudy

简介：作为在地震学，液体，热和精力的基本问题，地震附近的分发在地震产生期间采购原料是地震学者的担心的领先的题目。当前，越来越多的研究在地震来源区域附近显示出液体，它在地震准备和产生的过程起一个重要作用。然而，在在深外壳中的液体的来源上有可观的争吵。至于在地震来源区域附近的热的问题，不同模型被建议了向压力热流动解释悖论。在他们之中，动态变弱模型被认为是解决热流动悖论问题的关键。在大地震以后，精力分发是直接与磨擦热有关。立即深实现具有及时、重要的实际意义钻调查在地震产生期间获得液体，磨擦热和精力分发的理解的在里面地点。在液体，热和精力分发研究的最近的国际进步在将为地震准备和出现的理解带重要灵感的这篇论文被考察了。

简介：TheTanlu(Tancheng-Lujiang)faultisoneofthemajorstructuresineasternChina,whichcutsacrossdifferentblocksandcontrolsthetectonicactivity.UsingtheseismicdatafromtheChinaEarthquakeNetworksCenter,weinvestigatethespatialvariationsoftheb-valueintheDabie-Sulu(Jiangsu-Shandong)organicbeltbycalculatingtheb-valueofeachgrid(1°×1°)from1970to2010.Thestudyshowsthat:theb-valueissmallerintheTanlufaultanditsadjacentarea,whichmightsuggestthatthemajorearthquakerecurrenceperiodisrelativelylongduetothelowerfrequencyofsmallearthquakeactivity.InbothsidesofTanlufault,theb-valueishigherattheedgeofSulublockandtheeasternpartofDabieorogenicbelt.ThebvaluesarehigherinNorthChinacentralorogenicbelt,andsmallearthquakeactivitywhichoccurredalongthecentralorogenicbeltisfrequent.Additionally,combinedwithgeologicalandgeophysicalstudy,wefindthattheb-valuehasacertaincorrespondencerelationshipwiththelithologicdistribution,whichinformsusthatseismicactivityfeaturesarecloselyrelatedtotheinhomogeneousmediainthecrust.