The extensive use of depth-imaged seismic data produced by pre-stack depth migration(PSDM)leads to the necessity to synthesize seismogram directly in depth domain.However,since seismic wavelet in depth domain is depen...The extensive use of depth-imaged seismic data produced by pre-stack depth migration(PSDM)leads to the necessity to synthesize seismogram directly in depth domain.However,since seismic wavelet in depth domain is dependent on media velocities.The time-domain convolution operation directly used in depth domain does not meet the linear time-invariant condition.In this paper,we present a new method for genuine depth-domain seismic synthesis.This method constructs the velocity-dependent seismic wavelets varying adaptively with the corresponding interval velocities in the depth direction and weights them by the reflectivities,then the synthetic seismic record is obtained by the superposition of these weighted depth-varying wavelets.We applied this method to synthesize the seismic record of both a multi-layered geological model and the field data.The results show that the method can accommodate the intrinsic velocity-dependent variation characteristics of seismic events in depth domain and avoid the redundant depth-to-time and time-to-depth transformations.展开更多
文摘The extensive use of depth-imaged seismic data produced by pre-stack depth migration(PSDM)leads to the necessity to synthesize seismogram directly in depth domain.However,since seismic wavelet in depth domain is dependent on media velocities.The time-domain convolution operation directly used in depth domain does not meet the linear time-invariant condition.In this paper,we present a new method for genuine depth-domain seismic synthesis.This method constructs the velocity-dependent seismic wavelets varying adaptively with the corresponding interval velocities in the depth direction and weights them by the reflectivities,then the synthetic seismic record is obtained by the superposition of these weighted depth-varying wavelets.We applied this method to synthesize the seismic record of both a multi-layered geological model and the field data.The results show that the method can accommodate the intrinsic velocity-dependent variation characteristics of seismic events in depth domain and avoid the redundant depth-to-time and time-to-depth transformations.
