**Table 6.**

*Abu Roash dome area data and theoretical calculation parameters for model (1).*

later will be used for data calculating, tracing the formations' thicknesses, and depth's basement rocks along the profile line AA', by applying the proposed algorithm with Matlab's codes. In the final step, it found that the calculations for the two models along the profile line AA' are given the same results, as expected since the


*New Semi-Inversion Method of Bouguer Gravity Anomalies Separation DOI: http://dx.doi.org/10.5772/intechopen.101593*

**Table 7.**

*Abu Roash dome area data and theoretical calculation parameters for model (2).*


### **Table 8.**

*The thicknesses of formation: Along profile AA' in kilometers (*H *= Σh(*i*).* i *= 1, 2, 3, 4, and 5), Abu Roash dome area.*

calculated average vertical density-contrasts are the same for the two models. The results for the two models of Abu Roash Dome Area are summarized in **Tables 8** and **9** representing formations thicknesses, and depths, respectively, and represented graphically as shown in (**Figures 10** and **11**).
