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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: The Petroleum Potential of Egypt and
New Exploration
Opportunities
Opportunities
By
EGPC (Egyptian General Petroleum Corporation)
Cairo, Egypt
Since the onshore discovery of oil in the Eastern Desert in 1886, the petroleum industry in Egypt has discovered over 15.5 BBOE of reserves.
While the onshore Western Desert may contribute an additional
15-30 TCF in new future
resources
, the offshore Mediterranean
may hold an additional 64-84 TCF above the 25 TCF already
discovered, with many new fields in the giant class (>100
MMBOE). The current deep-water gas discoveries and activity are
relatively unique worldwide and hence may require a substantial
learning curve to understand how to drill, complete, develop and
optimize deepwater gas reservoirs in a cost-effective manner.
The offshore Gulf of Suez may yield an additional 1.5-3.3 BBOE. Advances in seismic multiple suppression and development of new "off-structure" play concepts with higher quality seismic data should result in continual new pool discoveries.
Frontier exploration offshore includes the Red Sea rift Province,
where deep water and sub-salt imaging remain significant
challenges
to overcome, and the Gulf of Aqaba.
More remote new exploration areas include the Komombo and other basins in Upper Egypt, currently under re-evaluation by a number of international oil companies.
Despite a relatively complex history, the geological framework of
Egypt is highly suited for oil and gas exploration. It comprises
eight major tectono-stratigraphic events:
1 ) Paleozoic craton
2 ) Jurassic rifting
3) Cretaceous passive margin
4) Cretaceous Syrian arc deformation and foreland transgressions
5) Oligo-Miocene Gulf of Suez rifting
6) Miocene Red Sea breakup
7) Messinian salinity crisis
8) Plio-Pleistocene delta progradation.
Each of these events has created multiple reservoir and seal combinations. Source rocks occur from the Paleozoic through to the Pliocene and petroleum is produced from Precambrian through Pleistocene age reservoirs.
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