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Depositional and Structural Styles in the Logone Birni Basin (LBB), Northern Cameroon, from 3D Potential Field Modeling: Preliminary Results

Depositional and Structural Styles in the Logone Birni Basin (LBB), Northern Cameroon, from 3D Potential Field Modeling: Preliminary Results

作     者:Elad Mkoumbe Fosso Téguia M. Estelle Eric Eyike Yomba Albert Njandjock Nouck Philippe Tabod Charles Tabod 

作者机构:Department of Physics Faculty of Science University of Douala Douala Cameroon Branch for Geophysical and Volcanological Research/Institute of Geological and Mining Research Buea Cameroon Department of Physics Faculty of Science University of Yaoundé I Yaoundé Cameroon 

出 版 物:《Open Journal of Geology》 (地质学期刊(英文))

年 卷 期:2019年第9卷第4期

页      面:226-244页

学科分类:1002[医学-临床医学] 100214[医学-肿瘤学] 10[医学] 

主  题:Gravity/Magnetic Anomalies Stratigraphic Sequences Sediment Thickness Logone Birini Basin 3D-Model 

摘      要:A three-dimensional model of the Logone Birni Basin (LBB) is presented by combining gravity and magnetic data and constrained by broad seismic profiles. The 3-D model has revealed the distribution of the stratigraphic formations as well as the top basement variation. Detailed structure of different stratigraphic sequences is presented for the first time for this basin and some of the sequences correlate with established sequences of the neighboring basins. The sediments pill consists of six sedimentary units dating from the Neocomian to the Quartenary. The Makary subbasin or Northern Logone Birni Basin (NLBB) is the deepest part of the basin and may hold good prospect for hydrocarbon generation and accumulation. However, the limited presence of faults and intrusive bodies decreases the possibility of thermal degeneration, contrary to the Central Logone Birni Basin (CLBB) where conditions seem to be fulfilled for possible hydrocarbon generation and maturity. The complexity of the structural pattern of the model is further enhanced by the presences of volcanic bodies, some of which lay directly on basement or interbedded with the sediments layers mainly in the CLBB.

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