Abstract
The goal of vibroseis data acquisition and processing is to produce seismic reflection data with a known spatially-invariant w avelet, preferably zero-phase, such that any variations in the data can be attributed to variations in geology. It is impossible to achieve this goal unless the data are deconvolved for the true ground force. Determination of the true ground force using current methods is at best approximate. A combination of approaches may lead to a more satisfactory approximation.
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