Crustal velocity structure of central Gansu Province from regional seismic waveform inversion using firework algorithm

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摘要 Thefireworkalgorithm(FWA)isanovelswarmintelligence-basedmethodrecentlyproposedfortheoptimizationofmulti-parameter,nonlinearfunctions.NumericalwaveforminversionexperimentsusingasyntheticmodelshowthattheFWAperformswellinbothsolutionqualityandefficiency.WeapplytheFWAinthisstudytocrustalvelocitystructureinversionusingregionalseismicwaveformdataofcentralGansuonthenortheasternmarginoftheQinghai-Tibetplateau.Seismogramsrecordedfromthemomentmagnitude(MW)5.4Minxianearthquakeenableobtaininganaveragecrustalvelocitymodelforthisregion.WeinitiallycarriedoutaseriesofFWArobustnesstestsinregionalwaveforminversionatthesameearthquakeandstationpositionsacrossthestudyregion,invertingtwovelocitystructuremodels,withandwithoutalow-velocitycrustallayer;theaccuracyofouraverageinversionresultsandtheirstandarddeviationsrevealtheadvantagesoftheFWAfortheinversionofregionalseismicwaveforms.WeappliedtheFWAacrossourstudyareausingthreecomponentwaveformdatarecordedbyninebroadbandpermanentseismicstationswithepicentraldistancesrangingbetween146and437km.Theseinversionresultsshowthattheaveragethicknessofthecrustinthisregionis46.75km,whilethicknessesofthesedimentarylayer,andtheupper,middle,andlowercrustare3.15,15.69,13.08,and14.83km,respectively.ResultsalsoshowthattheP-wavevelocitiesoftheselayersandtheuppermantleare4.47,6.07,6.12,6.87,and8.18km/s,respectively.
机构地区 不详
出处 《地震学报:英文版》 2017年2期
出版日期 2017年02月12日(中国期刊网平台首次上网日期,不代表论文的发表时间)
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