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Seismic waveforms and velocity model heterogeneity: towards full-waveform microseismic location algorithm

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Figure

Table 1: Event locations as computed using the eikonal solver. The 3 synthetic datasets were generated using the 3 velocity models
Figure 1:  Comparison of event locations using the eikonal solver with respective 90% confidence ellipses for a source with dominant source frequency of 300 Hz
Figure 2:  P-wave velocity model of the Horn River Basin reservoir used in the wide-angle simulations
Figure 3:  Vertical snapshot of wavefield after propagating a total distance of 250 m horizontally for N=2, 3, 4, 5, 6, and 7 number of velocity model interpolants, and the exact wide-angle solution
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