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Assessment of pore pressure in the Oligocene–Pleistocene stratigraphy of the West Delta Deep Marine, offshore Nile Delta, Egypt

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Abstract

One of the main drilling challenges in the offshore deep-water Nile Delta is the overpressured Tertiary shales, which causes formation fluid influxes, kicks, and very narrow drilling window, thus contributes to non-productive times and enhanced drilling risk. Accurate understanding of pore pressure distribution is crucial for casing design, mud optimization and safe and successful drilling. This study presents first ever in-depth analysis of the pore pressure distribution within the 4500 m thick Oligocene-Pleistocene stratigraphy from the West Delta Deep Marine block in deep-water Nile Delta. Direct formation pressure measurements indicated around 0.06–0.1 PSI/ft (1.36–2.26 MPa/km) gas gradient in the Pliocene El Wastani and Kafr El Sheikh sandstone reservoirs, while the Miocene Qantara sandstones are water-bearing with a 0.42 PSI/ft (9.5 MPa/km) pressure gradient. Shale porosity distribution exhibited additional porosity retention within the montmorillonite and mixed clay-dominated Late Pliocene and deeper sediments and marks the onset of overpressure at the top Kafr El Sheikh Formation. Based on the loading trends and acoustic slowness-density relationship, we inferred compaction disequilibrium as the primary overpressure generating mechanism resulted from high sedimentation rate. Shale pore pressure was interpreted by utilizing wireline logs by utilizing compaction trendline-based approach and calibrated with drilling events and mudlog data. Qantara and Tineh formations are characterized by 0.75–0.77 PSI/ft (16.96–17.41 MPa/km) pore pressure gradient leaving a narrow drilling mud window of 1.7–2 PPG. Based on vertical effective stresses, two significant overpressure compartments were identified in the Late Pliocene and Early Miocene-Late Oligocene, which were separated by the Middle Miocene Sidi Salem Formation acting as a pressure seal.

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Data availability

The data utilized in this study is confidential and cannot be shared publicly. Please contact the corresponding author in case of any queries.

Abbreviations

WDDM:

Western delta deep marine

Sv:

Vertical stress

Z:

Depth

TVD:

True vertical depth

ρw :

Density of sea water

ρ(Z) :

Bulk-density as a function of depth (Z)

g:

Gravitational acceleration

PP:

Pore pressure

RFT:

Repeat formation tester

NCT:

Normal compaction trend

Phyd :

Hydrostatic pore pressure

VES:

Vertical effective stress

Dt:

Acoustic slowness log

DtN:

Acoustic slowness of normally compacted shales

EDt:

Eaton’s exponent for acoustic slowness-based pore pressure estimation

R:

Resistivity log

RN:

Resistivity of normally compacted shales

ER:

Eaton’s exponent for resistivity-based pore pressure estimation

MW:

Mud weight

CG:

Connection gas

POG:

Pump-off gas

FP:

Fracture pressure

FG:

Fracture gradient

K0:

Effective stress ratio

LOT:

Leak-off test

FIT:

Formation integrity test

GWC:

Gas water contact

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Acknowledgements

Authors express their sincere gratitude to Hector Marin Moreno (Editor) for the excellent editorial handling and the two anonymous reviewers for their constructive reviews which benefited the manuscript. Authors acknowledge Egyptian General Petroleum Company (EGPC) for providing the dataset used in this study and permission to publish this work. Khaled Al-Kahtany acknowledges the Research Supporting Project Number RSP2024R139, King Saud University (Riyadh, Saudi Arabia).

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No funding was received for conducting this study.

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SS conceptualized the study, performed the formal analysis, and prepared the first draft of manuscript. All authors contributed to the data collection and curation, literature review, project management, review, and revision of the manuscript at various stages.

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Correspondence to Sherif Farouk or Souvik Sen.

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Farouk, S., Sen, S., Ahmad, F. et al. Assessment of pore pressure in the Oligocene–Pleistocene stratigraphy of the West Delta Deep Marine, offshore Nile Delta, Egypt. Mar Geophys Res 45, 6 (2024). https://doi.org/10.1007/s11001-023-09536-x

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