استفاده از تبدیل موجک بر روی داده های گرانی و تعیین عمق و شکل توده

One of the main objectives in interpretation of gravimetric data is determination of depth and structure of the mineral deposits. This article tries to use the wavelet transform as a new method for achieving such a goal. The advantage of this technique over traditional methods is the ability of differentiating the small and large anomalies easily by using windows of different sizes. In this paper we try to apply this method on gravimetric data, to find the depth and structure of the mineral deposits and compare the results of an artificial model with hypothetical one. This method has proved to be satisfactory at least for the one dimensional example mentioned above.