Abstract

The Abu Gabra and Bentiu formations are widely distributed within the interior Muglad Basin. Recently, much attention has been paid to study, evaluate and characterize the Abu Gabra Formation as a proven reservoir in Muglad Basin. However, few studies have been documented on the Bentiu Formation which is the main oil/gas reservoir within the basin. Therefore, 33 core samples of the Great Moga and Keyi oilfields (NE Muglad Basin) were selected to characterize the Bentiu Formation reservoir using sedimentological and petrophysical analyses. The aim of the study is to de-risk exploration activities and improve success rate. Compositional and textural analyses revealed two main facies groups: coarse to-medium grained sandstone (braided channel deposits) and fine grained sandstone (floodplain and crevasse splay channel deposits). The coarse to-medium grained sandstone has porosity and permeability values within the range of 19.6% to 32.0% and 1825.6 mD to 8358.0 mD respectively. On the other hand, the fine grained clay-rich facies displays poor reservoir quality as indicated by porosity and permeability ranging from 1.0 to 6.0% and 2.5 to 10.0 mD respectively. A number of varied processes were identified controlling the reservoir quality of the studies samples. Porosity and permeability were enhanced by the dissolution of feldspars and micas, while presence of detrital clays, kaolinite precipitation, iron oxides precipitation, siderite, quartz overgrowths and pyrite cement played negative role on the reservoir quality. Intensity of the observed quartz overgrowth increases with burial depth. At great depths, a variability in grain contact types are recorded suggesting conditions of moderate to-high compactions. Furthermore, scanning electron microscopy revealed presence of micropores which have the tendency of affecting the fluid flow properties in the Bentiu Formation sandstone. These evidences indicate that the Bentiu Formation petroleum reservoir quality is primarily inhibited by grain size, total clay content, compaction and cementation. Thus, special attention should be paid to these inhibiting factors to reduce risk in petroleum exploration within the area.

Highlights

  • The Great Moga together with Keyi oilfields of the Fula sub-basin are located in the northeastern region of the Muglad Basin (Fig. 1)

  • Thermal maturity assessment determined using vitrinite reflectance, biomarker parameters, pyrolysis gas chromatography and production index (PI) data indicated that the source rocks have reached the oil generation ­window[1,2,8,9]

  • Only little studies have been conducted on the Bentiu Formation despite being the major oil and gas reservoirs in the Muglad Basin

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Summary

Introduction

The Great Moga together with Keyi oilfields of the Fula sub-basin are located in the northeastern region of the Muglad Basin (Fig. 1). ­Authors[1,6,7,8] reported that, the Lower Cretaceous shales and claystones of the Abu Gabra Formations represent the primary source rocks within the Muglad Basin. These are mainly characterized by Type I kerogen with very good to excellent hydrocarbon generation potentials. Within the Fula Sub-Basin, clayey shales of the Abu Gabra Formation are very good source rocks. The Abu Gabra Sandstones, the thick Bentiu Formation sandstones as well as Aradeiba, Zarga and Ghazal sandstones (Darfur Group) are the major reservoir rocks, while claystones of Darfur Group serve as regional s­ eals[3,11,18]. Results of this study can be utilized to enhance the chances of success in the exploration activities within the region and other similar area around the world

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