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| Petroleum Licensing and Administration | ||
| Ministry of Mines and Energy | ||
| 2006 | ||
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Sedimentary rocks that occur in Basins of different geologic time cover over one-third of the surface area of Ethiopia. The Basins formed in the Upper Paleozoic-Lower Mesozoic are known as: the Ogaden, Abay (Blue Nile) and Mekele Basins, |
whereas those of the Upper Mesozoic to Middle Tertiary Basins are called the Gambela and Southern Rift Basins. Younger Tertiary rift grabens also occur all along the axis of the East African Rift System. |
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The Ogaden Basin, situated in the eastern part of Ethiopia, covers an area of about 350,000 sq. km. It contains thick sedimentary succession up to 10 km in the deeper parts, spanning Late Paleozoic to Early Tertiary. Lithologically the sediments comprise deep |
to shallow marine and continental sediments. There are two gas/condensate field discoveries in the Ogaden, namely Calub and Hilala. The Calub gas condensate reserve is estimated at 2.7 TCF and that of Hilala is about 1.3 TCF. |
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| Potential Source Rocks The main source rocks in the Ogaden Basin are represented by the Bokh Formation (Permo-Triassic), the transition zone (top Adigrat to base Lower Hamanlei, Early Jurassic) and the Uarandab Fm (Middle to Upper Jurassic), with source potential of 7 kg HC/t, 8.6-20 kg HC/t, and 5.3 kg Hc/t of rock respectively and their respective net thickness ranges up to 300 m, 120 m and 120 m. The hydrocarbons generated are mainly gas for Bokh Formation and oil and/gas for the others. Reservoir RocksRock units with good quality reservoir characteristics include the Calub Sandstone (Carboniferous/Permian), the Adigrat Sandstone (Late Triassic-Early Jurassic) and Middle and Upper Hamanlei Formations (Middle Jurassic, both of which are carbonate units). The Adigrat Sandstone (net thickness up to 135 m) has a porosity that ranges between 10% and 20%, with permeability that reaches up to 100 mD. The porosity and permeability qualities of the Upper Hamanlei |
are rather excellent- 20–23% porosity and permeability between 10 and 1000 mD. The Middle Hamanlei has porosity values between 12 and 26% and permeability of 5-6 mD. The Calub sandstone has a net thickness of up to 40 m and a porosity of 7%-20% with a permeability about 10 mD. Traps and Seal RocksDrag folds related with wrench tectonics, domal features and fault blocks have been identified as potential structural traps in several blocks of the Ogaden Basin. Stratigraphic trap conditions have also been recognized in the Mesozoic beds at the southwestern part of the Basin. The Uarandab Formation (mainly shale and marl) is a good regional seal unit for petroleum accumulated in the Upper Hamanlei reservoirs. Shale intercalations and evaporites (anhydrite) in the Middle Hamanlei are also good seal beds that overlie the reservoir units of the same Middle Hamanlei formation. The Permian Bokh Shale and the Transition Zone along with the lower Hamanlei tight carbonates and shale beds make good seal to the Calub and Adigrat reservoirs, respectively. |
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The Mesozoic Basins of Yemen with commercial oil reserves have corelatable sedimentary sequences to that of the Ogaden Basin. Oil and gas shows in several wells drilled in the Ogaden are promising and call for attention of identifying possible trap seal condition. Abay Basin (63,000 km2)Mesozoic Basin with sedimentary sequence comparable to that of the Ogaden. Upper Jurassic Antalo Limestone which is equivalent to Uarandab Formation in the Ogaden Basin is a potential source rock. A geochemical analysis of an oil seep sample from the northeastern end of the Basin (at Woreilu locality) indicated the presence of mature marine source rock. The Adigrat Sandstone, Amba Aradom Formation (Upper Sandstone) and some beds of the Antalo Limestone are considered potential reservoirs. Gambela BasinThis Basin, with an area of 17,500 sq. km, lies at the southeast extension of the White Nile Rift of the Sudan which contains the petroliferous Melut Basin. Upper Mesozoic to Palaeocene sediments reaching up to 5000m in thickness are expected to exist in fault-bounded grabens. |
Lacustrine shales and associated fluviatile sands are considered potential source and reservoir rocks in the Basin, respectively. Currently the Malaysian company known as PETRONAS CARIGALI is undertaking exploration over the entire expanse of the Basin. The Southern Rift BasinsThe Omo and Chew Bahir Basins along with other small size grabens that lie within the East African Rift System make up the Southern Rift Basins. From forward gravity modelling it is shown that 3000 to 3500 m thick sediment is expected in the depocenters of the larger Basins. The possible continuation of the older Mesozoic rifts of the Anza Graben of Kenya and the Abu Gabra Rift of the Sudan is also suggested in some studies. Mekele BasinsThe Basin covers an area of 8,000 sq. km and the Mesozoic sedimentary succession in this Basin is over 2000 m thick. The Adigrat Sandstone (150-160 m) is the potential reservoir, although, the presence of potential source rock is yet to be established. |
| Available Data | |
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| TERMS OF PETROLEUM AGREEMENT |
Petroleum agreement will be in the form of Model Production Sharing Agreement of 1994 or Modern Concession contract to be signed between the Government of Ethiopia, represented by the Minister of Mines, and a Contractor. BASIC PETROLEUM LEGISLATION:
ROYALITY, TAX AND RENTALS:
GAS PROVISIONS:
SIGNATURE:
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ADMINISTRATION:
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| Submission of Application |
Applications from individual companies as well as from groups of companies will be considered.
An application should be made to:
Minister (_________)
Ministry of Mines & Energy
P. O .Box 486.
Addis Ababa, Ethiopia
It should be submitted in a sealed envelope delivered by certified mail or hand. The envelop must be marked:
"Confidential"
"Proposal for Petroleum Exploration
and Production"
There is no payment of any application fee.
ii Content of an Application Presentation of applications shall be in accordance with the provisions of the following Section IV. All documents concerning an application shall be kept confidential by all parties. iii Inquiries Any information or clarification or the submission of an application may be obtained from: Petroleum Operations Department Ministry of Mines & Energy P. O. Box 486 Addis Ababa, Ethiopia Tel: 251-1-646-12-09 251-1-646-12-08 Fax: 251-1-646-34-39 or 251-1-646-33-64 After having examined the applications received, the Government may at its sole discretion invite a successful applicant to appear in Addis Ababa for negotiation. |
iv FORM OF PRESENTATION AND
CONTENT OF APPLICATION In assessing applications, the Government shall focus, among others, on the following: ADDIS ABABA, April 1994
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