Application of 3D Euler Deconvolution and 2D inverse modelling to basin depth estimation, the case of the Keta basin, Ghana | ||
| NRIAG Journal of Astronomy and Geophysics | ||
| Volume 9, Issue 1, January 2020, Pages 393-401 PDF (2.08 M) | ||
| DOI: 10.1080/20909977.2020.1743019 | ||
| Authors | ||
| Nuamah Daniel O. B.; Tandoh Kingsley K. | ||
| Abstract | ||
| 3D Located Euler Deconvolution and 2D Inverse Modelling have been applied to aero-magnetic and gravity data, respectively, to estimate depth to the basement across the Keta-basin, South-eastern Ghana, West Africa. The Euler deconvolution estimated relative depths, illustrated by depth solutions across the entire basin while the inverse modelling estimated the absolute depth at various positions in the basin. To improve and provide more accurate depth solutions, we applied the Located 3D Euler Deconvolution Method instead of the Standard Euler Deconvolution. The Located Euler depth estimate were obtained by calculating an analytic signal grid, finding peaks in the grid, then using the peak locations for located 3D Euler deconvolution. This method produced far lesser solutions than the Standard 3D Euler deconvolution. To estimate absolute depths across the basin, 2D inverse models were created along with five profiles constructed across strike on the gravity bouguer anomaly map. An Iterative Least Squares Inversion Method which is a non-linear inversion technique was applied to automatically calculate the model parameter (depths) in each step of the iteration process. The inversion procedure can easily be integrated with geologically realistic models. Comparatively, both methods produced similar depth estimates. The study showed higher depths to the south and east of the study area (>2 km) as the shallower depth occurs to the north (<2 km). The relative thickness of sedimentary succession was inferred from the depth distribution patterns as observed from Euler depth solutions. The highest depth estimated was 3.57 km which occur further south of the basin. | ||
| Keywords | ||
| Euler deconvolution; inverse Modelling; depth Measurements; Bouguer anomaly | ||
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