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Tidal and Drift Corrections: A Field Procedure

Let's now consider an example of how we would apply this drift and tidal correction strategy to the acquisition of an exploration data set. Consider the small portion of a much larger gravity survey shown below. To apply the corrections, we must use the following procedure when acquiring our gravity observations:

The procedure described above is generally referred to as a looping procedure with one loop of the survey being bounded by two occupations of the base station. The looping procedure defined here is the simplest to implement in the field. More complex looping schemes are often employed, particularly when the survey, because of its large aerial extent, requires the use of multiple base stations.



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