Euler Deconvolution Theory and Applications Part 1

Euler deconvolution is a geophysical method that uses potential field data to estimate the locations and depths of subsurface geological structures or anomalies.
It uses Euler's equation to describe the relationship between spatial derivatives of a potential field and the sources causing anomalies.
The method calculates Euler solutions, providing estimates of depths and locations of potential subsurface sources or anomalies.

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