Аннотации:
© SGEM2014 All Rights Reserved. In this study we present a method for interpretation of gravimetric data based on the socalled “native” wavelet basis. We show that this apporach has several distinct advantages over commonly used methods, including a simple way of obtaining formal solutions of the inverse problem, easy identification of the causative sources, and efficient search for solutions of the nonlinear inverse problem in the wavelet domain.