| 摘要 |
Methods and related apparatus for conducting shear slowness logging are set forth. The methods broadly comprise: detecting dispersive waves such as flexural or Stoneley waves; Fourier transforming the received signals; backpropagating the Fourier transformed signals according to equations using different dispersion curves; stacking the backpropagated signals; and finding semblances in order to choose the dispersion curve of maximum semblance and thereby identifying the shear slowness of the formation. Formation shear slowness may be plotted over borehole depth. Different embodiments are set forth. In one preferred embodiment (QDSTC), prior to Fourier transforming, the signals are stacked according to a previous estimation of slowness (S0), and are windowed for maximum energy. The reduced set of data in the window are then extracted for Fourier transformation, and prior to backpropagation, multiplied by S0 to reset them for backpropagation and stacking. In another preferred embodiment (DSTC), after the signals are backpropagated, the backpropagated signals are inverse fourier transformed and windowed. In DSTC, semblance values may be plotted as a function of slowness and time. Regardless of embodiment, the methods of the invention account for non-dispersive waves by using dispersion curves of constant value during backpropagation.
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