Abstract

Studies for the characterization of hydrocarbon reservoirs using well logs have been carried out in the M-Field of the Douala Basin to evaluate the hydrocarbon prospectivity, delineate hydrocarbon zones and determine the petrophysical properties of the identified reservoir rocks. Data from two wells comprising gamma ray, resistivity, neutron, density logs were used. Gamma ray log was used for lithologic discrimination; resistivity log was employed to identify formation fluid based on electrical responses of reservoir formations, while combined density and neutron logs were used to estimate reservoir porosity, as well as ascertain hydrocarbon type where present. Four hydrocarbon bearing reservoirs were delineated in the study area; one in Well-X (X2) with a thickness of 6.2 m and three others in Well-Y (Y1, Y2, Y3) with thicknesses of 19.2 m, 7.6 m and 78.7 m, respectively. Neutron–density crossplots indicate heterogeneous reservoir matrix comprising of sand, limestone and dolomite. The reservoirs were correlated using gamma ray log and were found to be discontinuous across the wells. The petrophysical parameters of the reservoirs evaluated indicate porosity, water-saturation and hydrocarbon-saturation values of X2 to be 20.8%, 30.8% and 69.2%, respectively, and the average porosity, water saturation and hydrocarbon saturation of the Well-Y reservoirs to be 40.2%, 18.3% and 81.7%, respectively. The porosity value indicates medium–high formation porosities and oil as the dominant hydrocarbon type. The crossplot of water-saturation and porosity revealed that the grain size variation of the reservoirs ranges from fine-grained to silty sands. The bulk volume water (BVW) values for the M-Field reservoirs suggest that they are homogeneous and at irreducible water saturation (Swirr) and hence will produce water-free hydrocarbons.

Highlights

  • The M-Field is an offshore field located within the Douala Basin

  • Journal of Petroleum Exploration and Production Technology (2019) 9:911–925 done or published data, regarding petrophysical analysis of wells in this field, the present study is aimed towards the petrophysical analysis of the rock units drilled in M-Field for evaluating the reservoir potential and establishing the stratigraphic relationship between the identified reservoirs encountered in these wells

  • The reservoirs in the study area could be described as calcareous quartz siltstones/sandstone within the N’kapa Formation due to the heterogeneous matrix which consists of fine-grained sand, limestone and dolomite

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Summary

Introduction

The M-Field is an offshore field located within the Douala Basin. The two wells of interest pseudo-named Well-X and Well-Y due to Cameroon’s National Hydrocarbon Corporation (SNH) confidentiality agreement were drilled; the1 3 Vol.:(0123456789)Journal of Petroleum Exploration and Production Technology (2019) 9:911–925 done or published data, regarding petrophysical analysis of wells in this field, the present study is aimed towards the petrophysical analysis of the rock units drilled in M-Field for evaluating the reservoir potential and establishing the stratigraphic relationship between the identified reservoirs encountered in these wells.Geological settingThe Douala/Kribi-Campo Basin located in the northern end of the South Atlantic is one of a series of divergent passive margin basins along the west coast of Africa, covering a total area of 19,000 km including 7000 km area which is located onshore (Pauken et al 1991). Journal of Petroleum Exploration and Production Technology (2019) 9:911–925 done or published data, regarding petrophysical analysis of wells in this field, the present study is aimed towards the petrophysical analysis of the rock units drilled in M-Field for evaluating the reservoir potential and establishing the stratigraphic relationship between the identified reservoirs encountered in these wells. The study area is located offshore and falls within the PH77 Prospect (Fig. 1). The deposits of this basin range from Cretaceous to Recent, the stratigraphy, as well as the sedimentology has been described in detail by Brownfield and Charpentier (2006) and Ntamak-Nida et al (2010), respectively. Eight litho-stratigraphic units which comprises the Mundeck, Logbadjeck, Logbaba, N’kapa, Souellaba, Kribi (Unnamed), Matanda and Wouri formations have been identified (Fig. 2). The formation is characterized mostly by stratigraphic trap (syns-sedimentary) mounds and sand sheet, as well as sub-unconformity traps formed beneath the Souellaba Formation Mid-Oligocene unconformity

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