A Comparative Geophysical Study of the Sedimentary-Metamorphic Contacts in the Douala and Kribi-Campo Sub-Basins of Cameroon

Nfor, Njingti; Clotilde, Owona Angue Marie Louise; Malquaire, Kue Petou Rokis; Eliezer, Manguelle-Dicoum; Achille, Lando Tsakou Julyo; Jöel, Piameu Kwagag

doi:10.31586/tjsr-3-1-4

Cited by 2 publications

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“…This previous work is necessary and provides a compass for future work. Despite these scientific advances in few regions [15][16][17][18][19], Cameroon in general and its southern part in particular faced peremptory energy deficit. In order to contribute a solution to this problem while preserving the environment, a correlative study based on the analysis of audio-magnetotelluric (AMT) and Landsat 8 satellite data measured with good spatial resolution (10 m to 5 m) is necessary to have more accurate and reliable information in the identification of potential geothermal sites.…”

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confidence: 99%

Identification of Geothermal Reservoirs in South Cameroon from a Combined Landsat 8 and AMT Data

Joel

Louise-Clotilde

Evariste

et al. 2022

International Journal of Geophysics

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This geothermal source prospecting work is carried out in order to respond to the energy deficit affecting the populations of South Cameroon in particular. The study combines audio-magnetotelluric (AMT) and Landsat 8 data for the geolocation of reservoirs, as well as the geological and tectonic information. The processing of these data defined 5 profiles and led to two-dimensional models of resistivity sections for each profile. The interpretation of the data identified a highly conductive zone with a resistivity ranged 1–10 Ω·m at an estimated depth of 1200 m in the locality of Menve’ele. The Landsat 8 data collected in this area during the same period enabled the elaboration of temperature and lineament anomaly maps of the study area. High-temperature areas with high lineament predominance correlate better with areas of low resistivity. For example, Menve’ele (A1) has a surface temperature range of 20°C–30°C and a high density of lineaments. By correlating these results with those provided by previous authors, the Menve’ele locality may be the target of a potential geothermal reservoir. A 3D resistivity model is built to better understand the variations of resistivity and their depths. The geological and tectonic information of the region confirm the tectonic origin of the faults and lineaments as well as the predominance of metamorphic and sedimentary formations.

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Section: Introductionmentioning

confidence: 99%

Identification of Geothermal Reservoirs in South Cameroon from a Combined Landsat 8 and AMT Data

Joel

Louise-Clotilde

Evariste

et al. 2022

International Journal of Geophysics

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Combination of Terrestrial and Satellite Gravity Data for the Characterization of the Southwestern Coastal Region of Cameroon: Appraisal for Hydrocarbon Exploration

Kamto

Lemotio

Tokam

et al. 2021

International Journal of Geophysics

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The southwestern coastal region of Cameroon is an area of interest because of its hydrocarbon potential (gas and oil). Terrestrial and satellite gravity data were combined and analyzed to provide a better precision in determining the structure of the study area. Firstly, the two gravity databases (in situ and satellite) have been coupled and validated using the least square collocation technique. Then, spectral analysis was applied to the combined Bouguer anomaly map to evaluate the thickness of sediments in some localities. We found that the sedimentary cover of the southwestern coastal region of Cameroon has a thickness that varies laterally from 1.68 ± 0.08 to 2.95 ± 0.15 km , especially in the western part. This result confirms that our target area is a potential site for hydrocarbon exploration. The horizontal gradient method coupled with the upward continuation at variable heights has been used to highlight several lineaments and their directions (N-S, E-W, SW-NE, and SSW-NNE). Lineaments trending in an N-S orientation are predominant. The Euler deconvolution method was also applied to the Bouguer anomaly map to determine the position, orientation, and depth of the different superficial faults of the study area. It appears that the majority of superficial faults have an N-S and SSW-NNE orientation. These directions are correlated with those previously highlighted by the maxima of horizontal gradient. The structural map could be used for a better identification of the direction of fluid flow within the subsurface or to update the geological map of our study area.

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A Comparative Geophysical Study of the Sedimentary-Metamorphic Contacts in the Douala and Kribi-Campo Sub-Basins of Cameroon

Cited by 2 publications

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Identification of Geothermal Reservoirs in South Cameroon from a Combined Landsat 8 and AMT Data

Identification of Geothermal Reservoirs in South Cameroon from a Combined Landsat 8 and AMT Data

Combination of Terrestrial and Satellite Gravity Data for the Characterization of the Southwestern Coastal Region of Cameroon: Appraisal for Hydrocarbon Exploration

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