Weighted Euler deconvolution of gravity data

摘要: Euler deconvolution is used for rapid interpretation of magnetic and gravity data. It particularly good at delineating contacts depth estimation. The quality the estimation depends mostly on choice proper structural index adequate sampling a function geometry causative bodies. For surveys, station distribution in general irregular, field aliased. This results erroneous estimates. By weighting equations by an error proportional to accuracies interstation distance, it possible reject solutions resulting from aliasing less accurate measurements. technique demonstrated Bouguer anomaly data Charlevoix region eastern Canada.