The Obs_Dip in Euler output datasets is defined as the dip from the current point of observation of the field to the calculated source body is a good filter for rejecting poorly conditioned solutions. The deconvolution process ensures there are clusters of solutions around the causitive bodies and those solution estimates that derive from further away for shallow bodies are suspect.
Created by: Evren Pakyuz-Charrier
Modified on: Mon, 9 Jul, 2018 at 11:35 PM
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