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作 者:Eric N. Ndikum Charles T. Tabod Eric N. Ndikum;Charles T. Tabod(Department of Physics, HTTC Bambili, The University of Bamenda, Bamenda, Cameroon;Department of Fundamental Sciences, Higher Technical Teacher Training College (HTTTC), Bamenda, Cameroon;Department of Physics, University of Yaoundé 1, Yaoundé, Cameroon;Department of Physics, Faculty of Science, The University of Bamenda, Bamenda, Cameroon)
机构地区:[1]Department of Physics, HTTC Bambili, The University of Bamenda, Bamenda, Cameroon [2]Department of Fundamental Sciences, Higher Technical Teacher Training College (HTTTC), Bamenda, Cameroon [3]Department of Physics, University of Yaoundé 1, Yaoundé, Cameroon [4]Department of Physics, Faculty of Science, The University of Bamenda, Bamenda, Cameroon
出 处:《Journal of Geoscience and Environment Protection》2023年第1期1-14,共14页地球科学和环境保护期刊(英文)
摘 要:The Gulf of Guinea constitutes an area of great petroleum potential yet with very limited geophysical research information. Consequently in this study, a Bouguer anomaly map has been computed from gravity data covering regions stretching from the Cameroon coastal basins to Bioko island (formerly Fernando Po) which is part of Equatorial Guinea. The data were further processed for Source Edge Detection (SED), Euler 3D deconvolution, 3D surface oriented models and 3D voxel solutions. The results confirmed the presence of previously identified intrusive bodies around the Douala and Kribi/Campo sedimentary sub-basins and went ahead to suggest a probable continuity between these two. A possible extension of this body offshore the Gulf of Guinea right up to Bioko island with very striking similarities was also highlighted and it shows characteristic variations in the depth to the surface of the body at different locations.The Gulf of Guinea constitutes an area of great petroleum potential yet with very limited geophysical research information. Consequently in this study, a Bouguer anomaly map has been computed from gravity data covering regions stretching from the Cameroon coastal basins to Bioko island (formerly Fernando Po) which is part of Equatorial Guinea. The data were further processed for Source Edge Detection (SED), Euler 3D deconvolution, 3D surface oriented models and 3D voxel solutions. The results confirmed the presence of previously identified intrusive bodies around the Douala and Kribi/Campo sedimentary sub-basins and went ahead to suggest a probable continuity between these two. A possible extension of this body offshore the Gulf of Guinea right up to Bioko island with very striking similarities was also highlighted and it shows characteristic variations in the depth to the surface of the body at different locations.
关 键 词:Intrusive Body 3D Surface-Oriented Model Gulf of Guinea
分 类 号:R38[医药卫生—医学寄生虫学]
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