简介:Thecommon-reflection-surface(CRS)stackingisanewseismicimagingmethod,whichonlydependsonseismicthreeparametersandnear-surfacevelocityinsteadofmacro-velocitymodel.AccordingtooptimizedthreeparametersobtainedbyCRSstacking,wederivedananalyticalrelationshipbetweenthreeparametersandmigrationvelocityfield,andputforwardCRSgathermigrationvelocitymodelingmethod,whichrealizevelocityestimationbyoptimizingthreeparametersinCRSgather.Thetestofasagmodelprovedthatthismethodismoreeffectiveandadaptableforvelocitymodelingofacomplexgeologicalbody,andtheaccuracyofvelocityanalysisdependsontheprecisionofoptimizedthreeparameters.