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The surface-consistent deconvolution applied at present can make spectrum decomposition in common shot point ( CSP) ��common receiver point ( CRP) ��common offset ( CO) and common midpoint ( CMP) domains to seismic record on the assumption of seismic wavelet being stable��but the attenuation effects of actual underground medium are not considered�� In order to truely reflect the reflection characteristics of underground medium�� Gabor surface-consistent deconvolution of seismic record has been processed in time-frequency domain�� This method can eliminates the effects of the wavelet excitation��acception effect and formation attenuation simultaneously�� Using offset and common midpoint information��the Q function component of deconvolution operator can be parameterized�� and estimates the seismic source excitation��geophone acception and formation attenuation in offset and common midpoint domain�� This method applied in data processing of Luzong concentration area has strong antinoise�� phase adaptation and thin-bed reflection compared with other surface-consistent deconvolutions��which overcomes the phenomena of frequency overcompensation or nonuniformity in different time-windows of the same wave group in spatial domain��and improves the resolution of seismic singal��