Abstract

Simultaneous seismic inversion and extended elastic impedance (EEI) were applied to obtain quantitative estimates of porosity, water saturation, and shale volume over Nianga field of Congo basin, West Africa. The optimum angle at which EEI log and the target petrophysical parameter give the maximum correlation was meticulously analyzed by additionally incorporating the concept of relative rock physics. Prestack seismic data were simultaneously inverted into Vp, acoustic, and gradient impedances. The last two broadband inverted volumes were projected to Chi angles corresponding to the target petrophysical parameters, and three broadband EEI volumes were obtained. At well control points, the linear trends based on specific lithology between EEI and petrophysical parameters were then used to transform EEI volumes into quantitative porosity, water saturation, and shale volume cubes. In order to obtain the reservoir facies distribution, another concept of minimum energy angle was used to generate the background EEI cube, thereby enabling the mapping of reservoir facies. From quantitative porosity, water saturation, shale content, and background EEI cubes, favorable zones have been pinpointed which may suggest possible drilling locations for future development of the field.

Highlights

  • Block 18 is situated in the southernmost portion of the lower Congo basin (Fig. 1)a Tertiary depocentre along the West African passive continental margin and is a product of Late Jurassic to Early Cretaceous rifting which heralded the first stage in the eventual opening of the southern Atlantic

  • The linear trends based on specific lithology between extended elastic impedance (EEI) and petrophysical parameters were used to transform EEI volumes into quantitative porosity, water saturation, and shale volume cubes

  • The proposed methodology aims at estimating tuned EEI cubes which approximately correspond to minimum background energy and petrophysical parameters such as porosity, water saturation, and shale volume cubes

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Summary

Introduction

Block 18 is situated in the southernmost portion of the lower Congo basin (Fig. 1)a Tertiary depocentre along the West African passive continental margin and is a product of Late Jurassic to Early Cretaceous rifting which heralded the first stage in the eventual opening of the southern Atlantic. The Nianga field is located in deep water in the north central region of Block 18, approximately 175 km offshore to the northwest of Luanda, and is separated from the neighboring Mamba field to the immediate west by a structural saddle and a stratigraphic pinch out. It is the largest field within the block development area, with estimated recoverable reserves greater than 250 MMBO. Sin v, q = -8K sin v, and r = cos v - 4K sin v, and Vp0, Vs0 and q0 are normalization factors of Vp (P-velocity), Vs (S-velocity), and q (density), respectively. Ð2Þ where AI0 is the normalization factor of AI (P-impedance) and GI is the gradient impedance.

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