This work includes a qualitative interpretation of gravity data over the area under studying which lies in the Western Desert of Egypt and also make a model for this data. Qualitative interpretation includes a separation of anomalies at two levels one and two Kilometers. These separations include drawing a maps of residual, regional and second derivatives at two levels (one and two Kilometers). Also, at this work we make a model for the gravity data using a trapezoidal model because this model can be used at the case of sedimentary rocks and the area under studying, from a geological data, contains also a sedimentary rocks.
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