Curie Point Depth from Spectral Analysis of Magnetic Data in Potiskum and Environs, Yobe State, Nigeria

Abstract

The area under investigation, is part of Chad basin of northeastern Nigeria, located between latitudes 11o00´ to 12o00´N and Longitudes  11o30´ to 12o30´E, with the objective to discover more about the thermal structure of the crust in the area, a research was carried out over  Potiskum and surrounding regions in Yobe State, Nigeria to estimate the curie point depth, geothermal gradient, and heat flow using  spectrum analysis and empirical formula of aeromagnetic data. To acquire the regional and residual data, polynomial fitting was applied  to the high-resolution digital aeromagnetic data. In order to calculate the depth to the centroid and the depth to the top boundary, the  upward continued residual data was processed to produce the upward continued data, that was subjected to spectral analysis. The depth  to the centroid is between 10.50 and 11.50 kilometers, the depth to the top boundary is between 5.90 and 7.16 kilometers, the depth to  the Curie point is between 14.84 and 16.83 kilometers, the geothermal gradient is between 34.462 and 39.083 oCkm-1, and the heat flow  is between 86.135 and 97.707 mWm-2. The Curie point depth inferred from the study indicates that the crust is thinning due to thermal  upwhirling of magma and is moderately decreasing toward areas of volcanic activity that occurred in the area during the Tertiary Period.  The Geothermal gradient shows that the area is a moderate temperature zone, which could likely result in partial thermal maturation of  sediments and hence probable oil generation as time goes on with an increase in temperature. In the research area, the geothermal  gradient is proportional to the heat flow, whereas the connection between curie depth and heat flow is inversely linear. These findings  are in line with the geotectonic regime that is now in effect in the research area. However, this analysis shows that the heat flow that was  obtained from the study is sufficient to be utilized as a geothermal energy source.