Under a fixed seismic frequency, wavelet side lobes may increase the difficulty of interpreting and recognizing thin sand bodies.
在地震资料频率一定的情况下，地震子波旁瓣效应会增加薄砂岩识别和解释的难度。
Under a fixed seismic frequency, wavelet side lobes may increase the difficulty of interpreting and recognizing thin sand bodies.
在地震资料频率一定的情况下，地震子波旁瓣效应会增加薄砂岩识别和解释的难度。
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