Abstract
The technique of processing gravimetric data is offered in this study. Offered technique based on wavelet transform with so-called Ā«nativeĀ» wavelet basis functions. Distinctive feature of the technique is a close relationship with both direct and inverse problems of gravimetry. It was shown that the peculiarity allows to quite simply and quickly location of causative sources even under of strong interference of gravity fields. Keywords: gravimetry; wavelet transform; anomaly; inverse problem.
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