摘要: Summary. Synthetic seismic tomographic data sets for cross-hole and hole-to-surface arrays are computed inverted. Inversion (imaging) is performed through an iterative projection solution to a matrix equation. The orientation as well the position of anomaly relative source recorder affects both rate convergence resolution obtained. Data density distribution determine physical validity image obtained at convergence. Borehole tomography apparently viable method imaging inter-hole structure.
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