Key challenges to realizing full potential in an emerging giant gas province: Nile Delta/Mediterranean offshore, deep water, Egypt

Author:

DOLSON J. C.1,BOUCHER P. J.2,SIOK J.3,HEPPARD P. D.3

Affiliation:

1. BP, Chertsey Road, Sunbury-on-Thames TW16 7LN, UK (e-mail:Dolsonjc@bp.com)

2. BP, 501 Westlake Park Blvd., Houston, TX 77253, USA

3. BP-Egypt, 14 Road 214, Maadi/Digla, Cairo, Egypt

Abstract

The Nile Delta is an emerging giant gas province with proven reserves of approximately 42 × 1012SCF. This resource has more than doubled in the last three years, largely from successful deep water exploration for Pliocene slope-channel systems. Proven reservoirs vary in age from Oligocene through Pleistocene. Source rocks include Jurassic coals and shales and the Lower Miocene condensed Qantara Formation shales. Additional source rocks may be present in condensed intervals of Cretaceous, Oligocene and Eocene age.Following Tethyan rifting and opening of the Mediterranean in the Jurassic, prominent Cretaceous mixed clastic and carbonate shelf edges aggraded vertically along a steep fault-bounded shelf-slope break (the ‘hingeline’) in northern Egypt, which exerts the fundamental control on reservoir distribution in Tertiary age strata. In late Eocene time, northern Egypt was tilted toward the Mediterranean during regional uplift associated with the opening of the Gulf of Suez and Red Sea rifts. Drainage systems shed reservoir quality sediments northward in a series of forced regressions. These regressions culminated in be-heading of the youngest deltas by subaerial erosion during the Messinian salinity crisis. Early Pliocene transgressions laid a thick sealing interval over the low-stand Messinian valley networks. Renewed deltaic deposition began at approximately 3.8Ma.The steep structural hingeline and faulted continental shelf created a large amount of accommodation space with relatively minor progradation of depositional systems. As a result, the primary play consists of slope-channel fairways in all levels. The Pliocene systems are the shallowest targets in the basin and future large reserve growth will come from the pre-Messinian strata.Nile Delta gas resources lie close to emerging and established markets in the Mediterranean. Challenges to capturing the deeper pre-Messinian prize include:establishing favourable economic terms for export and domestic markets;reducing drilling costs and optimization of wellbore patterns to develop multiple stacked objectives;working in deep water and high pressure environments;developing predictive models for pressure regressions in overpressured reservoir fairways;recognizing and exploiting thin bedded low resistivity pay.

Publisher

Geological Society of London

Subject

Fuel Technology,Energy Engineering and Power Technology,Geology,Geochemistry and Petrology

Reference26 articles.

1. Ayyad M. H. Darwish M. 1996. Syrian Arc structure: a unifying model of inverted basins and hydrocarbon occurrences in North Egypt. In: Youssef M. (ed.) Proceedings of the 13th Petroleum Conference, Cairo, Egypt, The Egyptian General Petroleum Corporation, 40–59.

2. Hydrocarbon exploration in a complex incised valley fill: An example from the late Messinian Abu Madi Formation (Nile Delta Basin, Egypt)

3. Egypt in the twenty-first century: petroleum potential in offshore trends;Dolson;GEOARABIA,2000

4. Dolson J. C. Shann M. V. Matbouly S. Harwood C. Rashed R. Hammouda H. 2001. The Petroleum Potential of Egypt. In: Downey M. W. Threet J. C. Morgan W. A. (eds) Petroleum Provinces of the 21st Century. American Association of Petroleum Geologists, Tulsa, Oklahoma, 453–482.

5. Dolson J.C. Barkooky A.E. Wehr F. Gingerich P. Prochazka N. Shann M. 2002a. The Eocene and Oligocene Paleo-Ecology and Paleo-Geography of Whale Valley and the Fayoum Basins: Implications for Hydrocarbon Exploration in the Nile Delta and Eco-Tourism in the Greater Fayoum Basin. American Association of Petroleum Geologists, Search and Discovery Article #10030: http://www.searchanddiscovery.com/documents/cairo/index.htm.

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