简介:Wienerfilteringisusedtoestimatereceiverfunctioninatime-domain.Withtheverticalcomponentof3-componentteleseismicPwaveformastheinputofaWienerfilter,receiverfunctionasthefilterresponse,andradialandtangentialcomponentsastheexpectedoutput,receiverfunctionisestimatedbyminimizingtheerrorbetweenexpectedandactualoutputs.ReceiverfunctioncanbeobtainedbysolvingtheToeplitzequationusingtheLevinsonalgorithm.Thenon-singularityoftheToeplitzequationensuresthestabilityofWienerDeconvolution.BothsyntheticandobservationalseismogramcheeksshowthatWienerDeconvolutionisaneffectivetime-domainmethodtoestimatereceiverfunctionfromteleseismicPwaveform.
简介:Ithasbeenwellstudiedthattheγ-functionexplicitmethodcanbeeffectiveinprovidingfavorablenumericaldissipationforlinearelasticsystems.However,itsperformancefornonlinearsystemsisunclearduetoalackofanalyticalevaluationtechniques.Thus,anoveltechniqueisproposedhereintoevaluateitsefficiencyforapplicationtononlinearsystemsbyintroducingtwoparameterstodescribethestiffnesschange.Asaresult,thenumericalpropertiesanderrorpropagationcharacteristicsoftheγ-functionexplicitmethodforthepseudodynamictestingofanonlinearsystemareanalyticallyassessed.Itisfoundthattheupperstabilitylimitdecreasesasthestepdegreeofnonlinearityincreases;anditincreasesasthecurrentdegreeofnonlinearityincreases.Itisalsoshownthatthisintegrationmethodprovidesfavorablenumericaldissipationnotonlyforlinearelasticsystemsbutalsofornonlinearsystems.Furthermore,errorpropagationanalysisrevealsthatthenumericaldissipationcaneffectivelysuppressthesevereerrorpropagationofhighfrequencymodeswhilethelowfrequencyresponsesarealmostunaffectedforbothlinearelasticandnonlinearsystems.
简介:Inthisarticle,weanalyzethecharactersofSV-componentreceiverfunctionofteleseismicbodywavesanditsadvantagesinmappingtheS-wavevelocitystructureofcrustindetail.Similartoradialreceiverfunction,SV-componentreceiverfunctioncanbeobtainedbydirectlydeconvolvingtheP-componentfromtheSV-componentofteleseismicrecordings.OuranalysesindicatethatthechangeofamplitudeofSV-componentreceiverfunctionagainstthechangeofepicentraldistanceislessthanthatofradialreceiverfunction.Moreover,thewaveformofSV-componentreceiverfunctionissimplerthantheradialreceiverfunctionandgivesprominencetothePSconvertedphasesthatarethemostsensitivetotheshearwavevelocitystructureintheinversion.ThesynthetictestsshowthattheconvergenceofSV-componentreceiverfunctioninversionisfasterthanthatoftheradialreceiverfunctioninversion.Asanexample,weinvestigatetheS-wavevelocitystructurebeneathHIAstationbyusingtheSV-componentreceiverfunctioninversionmethod.
简介:Basedonthefittingonpaleoearthquakedataofintra-plateregionsinthenorthernpartofChi-naandgivingastatisticalmodeloftimeinterdependence,thepotentialdamageearthquakesinadefinitefutureperiodandcharacteristicsofpresentshocksalongtheLingwufaulthavebeenanalyzedbyusingdangerousprobabilityfunctionandsomenewdataconcerned.Wehavein-ferredthatthefaulthasenteredaperiodthatearthquakeswillprobablyoccur.ThereexistsapotentialdangerthatastrongearthquakewithMs7.0-7.5willoccurin10-100a.