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Kirchhoff型反偏移场稳相分析(英文) Kirchhoff-typeAntimigrationPhaseAnalysis Introduction: Inexplorationseismology,seismicmigrationisaprocessinwhichrecordeddataistransformedintoanimageofthesubsurfacegeologicalstructures,bycorrectingforvariousdistortionscausedbythesubsurfacescatteringandtheacquisitiongeometry.However,incertaincases,migrationcanleadtoartifactsandinaccurateresults,duetothepresenceofcomplexsubsurfacestructures,suchasfaults,saltdomes,orgeologicalboundaries.Onewaytoavoidtheseissuesisthroughtheuseofphaseanalysistechniques,whichapproachmigrationfromadifferentperspective,byfocusingonthepropagationcharacteristicsoftheseismicwavefield.TheaimofthispaperistopresentaphaseanalysisalgorithmbasedonKirchhoff-typereverse-timemigration,thatcanbeusedtoobtainimagesofthesubsurfaceinchallenginggeologicalsettings. Kirchhoff-typeAntimigration: ThebasicprinciplebehindtheKirchhoff-typeantimigrationalgorithmistocomputethephaseofthemigratedwavefield,anduseittoundothemigrationprocess.Thisisachievedbydefininganewwavefieldastheproductofthemigratedwavefieldandanantiphase(complexconjugate)function,whichisdesignedtocanceloutthemigrationartifacts.Morespecifically,theantiphasefunctioniscomputedbytakingtheinverseFouriertransformofthephaseofthemigratedwavefield,andthenapplyinga2DGaussianwindowtosmoothoutthehigh-frequencycomponents.Theresultingfunctionisthenmultipliedwiththemigratedwavefield,beforeapplyingtheinversemigrationoperator,toobtainanimagethatisfreeofmigrationartifacts. StablePhaseAnalysis: Thekeyadvantageofthephaseanalysisapproachisitsabilitytohandlecomplexsubsurfacestructures,withoutintroducingmigrationartifacts.Thisisbecausethephaseofthewavefieldisaglobalproperty,thatisrelatedtothetraveltimeoftheseismicwaves,andhenceinsensitivetolocalperturbations.Therefore,eveninthepresenceofstrongvelocitycontrastsorcomplexboundaries,thephaseanalysisalgorithmcanproducestableandaccurateimagesofthesubsurface.Moreover,theuseofKirchhoff-typemigrationallowsforflexibilityinthemigrationstrategy,whichcanbeadaptedt