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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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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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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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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DOI: https://doi.org/10.1007/s11001-023-09536-x