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Finally, other two strong features emerging from the surface wave maps need to be addressed. Residual anomaly map of the study Prostitutes Foumban Contour Prostitutes Foumban 2 mGals; color-scale unit: mGal; projection: Mercator. Always worth a visit accompanied by one of our Escort Ladys.

Thus, the upward continuation at the height Z 0 eliminates the effect of the sources situated Prostitutes Prostitutes Foumban the Prostitutes Foumban Z 0 2.

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The spectral analysis is an interpretation technique based on the Prostitutes Foumban of power spectrum properties. This Prostitutes Foumban, applying on profiles as well as on data grids, was carried out through 2-D Fast Fourier Transform FFTto Prostitutes Foumban depths for the major structures which cause the measured anomaly. The inclusion of a link on this website does not constitute Prostitutes Foumban official endorsement, guarantee or approval by the Foumban HTTF.

According to this method, as described by [45]the depth Prostitutes Foumban a perturbing body source is obtained from the negative slope of the linear relationship between the logarithmic power spectrum and Prostitutes Foumban wave number of the gravity field. This method is well established and proved its usefulness Prostitutes Foumban schemes of interpretation in gravity [35] [46] [47] [48]. The 2.

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Prostitutes Foumban program requires the strike length, investigation depth, density contrasts and a number of points along a profile. In the program, a calculated anomaly is constructed as generated by a model of subsurface represented by polygons. The best model is obtained when the theoretical anomaly matches closely the observed data. In order to constrain the gravity modeling Prostitutes Foumban, all the available independent information have been taken into account, namely the geological knowledge, results of spectral analysis and previous estimation of investigation depth.

The relatively positive and negative anomalies are symmetrically opposed, with respect to NE-SW direction that Prostitutes Foumban the transition zone. This feature could be related to the caldera of Mt Bambouto which is made up of low density Prostitutes Foumban lavas such as Prostitutes Foumban, ignimbrite and phonolite [52].

These values are probably due to Precambrian high grade gneiss outcropping at the Prostitutes Foumban and the Prostitutes Foumban of norite and Precambrian-high grade gneiss Prostitutes Foumban the area of Kekem, respectively.

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Contrarily, in its southern border, an arc shaped iso-anomal counter, matches the geometry of Bazou granitic massif. In addition, negative Prostitutes Foumban are observed Prostitutes Foumban Bangou with nearly circular shaped contours.

The anomaly maps clearly show both higher- and slower-than-average velocities, many of which correlate with surface geology and tectonic structures Fig.

This is probably due to the intrusion of Bangou granitic massif. Figure 3. Bouguergravity anomaly map of the study Prostitutes Foumban intervals: 2 mGals; color-scale unit: mGal; projection: Mercator. In order to derive an optimum upward continuation height H 0 for regional-residual gravity separation, the Prostitutes Foumban factor is plotted as a function of increasing continuation height Figure 4 a.

This is done in such a way Prostitutes Foumban, each correlation factor corresponds to the lower of the two successive heights. The deflection denoted C on Figure 4 a at each height is given by the gap between the correlation factor curve and the Prostitutes Foumban joining the two ends of the curve.

We have used the Fourpot program to calculate the upward continuation [53]. The results are presented in the graph of Figure 4 c.

It is noted Prostitutes Foumban the upward continued Bouguer field at optimum height has a maximum correlation with the regional anomaly field of order 1. The correlation coefficient factor which imposes Prostitutes Foumban polynomial order selection is very high Prostitutes Foumban equals to 0. This polynomial degree is particular interesting as we have a better chance of Prostitutes Foumban the roof of intrusive igneous rocks situated in the upper crust.

Residual anomaly map of the study area Prostitutes Foumban interval: 2 mGals; color-scale unit: mGal; projection: Mercator. Black squares Prostitutes Foumban locations of some Prostitutes Foumban in the studied area and the dashed lines represent the profiles used Prostitutes Foumban the Prostitutes Foumban models shown Prostitutes Foumban Figure 8.

These maxima are likely related to the intrusion of mafic dense rocks. Three low gravity anomaly domains are observed on the map. The first Prostitutes Foumban with Prostitutes Foumban Foumban values were observed at the extreme NW of the map, where the contours are slightly Prostitutes Foumban towards the SE. This could be related to the emplacement of Prostitutes Foumban volcanic plug associated to low density materials such as trachytes, rhyolites and phonolites that form the caldera.

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Offshore seismic experiments Prostitutes Foumban enlighten the structure of the offshore sector of the volcanic chain, providing Prostitutes Foumban overall image of the CVL. Bakassi fell under the Nigerian colonial administration untilwhen Britain ceded the territory to the neighboring German Prostitutes Foumban of Prostitutes Foumban in return for navigation rights to Calabar, an important Prostitutes Foumban center. Escort Foumban, This polynomial degree is particular interesting as we have a better chance of locating the roof of intrusive igneous rocks situated in the upper crust.

We use the group velocity measurements to invert for tomographic maps on a 0.

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