The AWITM and FWI waveform inversion cost functions are applied to raw seismic field data for velocity model weight optimisation in an exploration block in the Central Atlantic margin. The key objective is to extend the main benefits of wave equation inversion to below the diving wave limit whilst using the fewest number of iterations. Employing the two stated cost functions, the automated model building gives well resolved velocity values over a kilometre below the diving wave limit as necessary to cover the target area for prospect maturation in the survey area.
High frequency model evolution
Iterations are run on 50 metre then 25 metre grids for broadband velocity recovery from long to short length scales with no gap between tomography and reflectivity. A total of 40 iterations are run upto 10 Hz, then 30 iterations upto 20 Hz. At iteration 70 the target layer at 3km depth is being defined and we decide to push the inversion for 15 more iterations on a 12.5 metre grid with frequencies upto 40 Hz. This requires 36 core EC2 instances to keep iteration times down to 90 mins.
The final model shows tilted fault block definition at target level with interbedded sand and shale layers. The fine scale detail also shows direct conformance with the vintage PSDM stack amplitude anomalies as the earth reflectivity is mapped into the rock property domain successfully.
Model predicted traces
The updating of the traces predicted by the model weights in relation to the field recorded traces show the inversion is being driven by refraction and reflection energy and the misfit is being minimised to the global minimum of the search space.
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