Affiliations 

  • 1 College of Earth Sciences, Jilin University, Changchun, 130061, China. makeen.geo@hotmail.com
  • 2 College of Earth Sciences, Jilin University, Changchun, 130061, China
  • 3 Department of Geology, University of Malaya, 50603, Kuala Lumpur, Malaysia
  • 4 Department of Geology, Federal University Lokoja, P. M. B 1154, Lokoja, Nigeria
  • 5 College of Earth Sciences, Jilin University, Changchun, 130061, China. ssyuan@jlu.edu.cn
  • 6 Jiangxi Engineering Laboratory on Radioactive Geoscience and Big Data Technology, East China University of Technology, Jiangxi, China
  • 7 Pan African University-Life and Earth Science Institute, University of Ibadan, Ibadan, Nigeria
  • 8 School of Earth Sciences, Northeast Petroleum University, Daqing, 163318, China
Sci Rep, 2021 09 16;11(1):18442.
PMID: 34531468 DOI: 10.1038/s41598-021-97994-x

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.

* Title and MeSH Headings from MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine.