Geological Modeling of Dahomey and Liberian Basins

The objective of this thesis is to study two Basins of the Gulf of Guinea (GoG), namely the Dahomey and the Liberian Basins. These Basins are located in the northern part of the GoG, where oil and gas exploration has significantly increased in the last 10 years or so. We proposed geological descript...

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Main Author: Gbadamosi, Hakeem B.
Other Authors: Ikelle, Luc T.
Format: Others
Language:en_US
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264
http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264
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spelling ndltd-tamu.edu-oai-repository.tamu.edu-1969.1-ETD-TAMU-2009-05-2642013-01-08T10:39:11ZGeological Modeling of Dahomey and Liberian BasinsGbadamosi, Hakeem B.DahomeyLiberianBasinsGulf of GuineaPlate tectonicsGeological modelsPinch-outsChannelsFinite-differencePre-Stack Depth Migration (PSDM)Shot-gathersZero-offset gathersThe objective of this thesis is to study two Basins of the Gulf of Guinea (GoG), namely the Dahomey and the Liberian Basins. These Basins are located in the northern part of the GoG, where oil and gas exploration has significantly increased in the last 10 years or so. We proposed geological descriptions of these two Basins. The key characteristics of the two models are the presence of channels and pinch-outs for depths of between 1 km and 2 km (these values are rescaled for our numerical purposes to 600- m and 700-m depths) and normal faults below 3 km (for our numerical purposes we use 1 km instead of 3 km). We showed that these models are consistent with the plate tectonics of the region, and the types of rocks and ages of rocks in these areas. Furthermore, we numerically generated seismic data for these two models and depth-migrated them. We then interpreted the migrated images under the assumption that the geologies are unknown. The conclusions of our interpretations are that we can see clearly the fault systems in both models. However, our results suggest that seismic interpretations of the channels and pinch-outs associated with the geology of the Dahomey and Liberian Basins will generally be difficult to identify. In these particular cases, we missed a number of channels and pinch-outs in our interpretations. The limited resolution of seismic images is the key reason for this misinterpretation.Ikelle, Luc T.2010-01-16T00:04:10Z2010-01-16T00:04:10Z2009-052010-01-16T00:04:10ZBookThesisElectronic Thesisapplication/pdfhttp://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264en_US
collection NDLTD
language en_US
format Others
sources NDLTD
topic Dahomey
Liberian
Basins
Gulf of Guinea
Plate tectonics
Geological models
Pinch-outs
Channels
Finite-difference
Pre-Stack Depth Migration (PSDM)
Shot-gathers
Zero-offset gathers
spellingShingle Dahomey
Liberian
Basins
Gulf of Guinea
Plate tectonics
Geological models
Pinch-outs
Channels
Finite-difference
Pre-Stack Depth Migration (PSDM)
Shot-gathers
Zero-offset gathers
Gbadamosi, Hakeem B.
Geological Modeling of Dahomey and Liberian Basins
description The objective of this thesis is to study two Basins of the Gulf of Guinea (GoG), namely the Dahomey and the Liberian Basins. These Basins are located in the northern part of the GoG, where oil and gas exploration has significantly increased in the last 10 years or so. We proposed geological descriptions of these two Basins. The key characteristics of the two models are the presence of channels and pinch-outs for depths of between 1 km and 2 km (these values are rescaled for our numerical purposes to 600- m and 700-m depths) and normal faults below 3 km (for our numerical purposes we use 1 km instead of 3 km). We showed that these models are consistent with the plate tectonics of the region, and the types of rocks and ages of rocks in these areas. Furthermore, we numerically generated seismic data for these two models and depth-migrated them. We then interpreted the migrated images under the assumption that the geologies are unknown. The conclusions of our interpretations are that we can see clearly the fault systems in both models. However, our results suggest that seismic interpretations of the channels and pinch-outs associated with the geology of the Dahomey and Liberian Basins will generally be difficult to identify. In these particular cases, we missed a number of channels and pinch-outs in our interpretations. The limited resolution of seismic images is the key reason for this misinterpretation.
author2 Ikelle, Luc T.
author_facet Ikelle, Luc T.
Gbadamosi, Hakeem B.
author Gbadamosi, Hakeem B.
author_sort Gbadamosi, Hakeem B.
title Geological Modeling of Dahomey and Liberian Basins
title_short Geological Modeling of Dahomey and Liberian Basins
title_full Geological Modeling of Dahomey and Liberian Basins
title_fullStr Geological Modeling of Dahomey and Liberian Basins
title_full_unstemmed Geological Modeling of Dahomey and Liberian Basins
title_sort geological modeling of dahomey and liberian basins
publishDate 2010
url http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264
http://hdl.handle.net/1969.1/ETD-TAMU-2009-05-264
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