摘要
The onset function is introduced to extend the traditional formation conversion model, and the singularity data is used to quantify the transit characteristics of the formation velocity. Moreover, the traditional convolution model is used to identify the transmission of the singularity data from acoustic impedance to composite seismogram. The singularity characteristics of formation medium are preserved in the seismogram and they can be considered as a natural seismic attribute that can delineate the formation boundaries accurately. With the mono-scale fractional-order Gaussian wavelet transformation algorithm, the wavelet transform modulus maximum points are traced by taking the disappearance or appearance of the maximum as the criterion for singularity index calculation.