Benisuef Basin the Key for Exploration Future Success in Upper Egypt
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Beni Suef Basin the Key for Exploration Future Success in Upper Egypt*
Hemida Zahran1, Khaled Abu Elyazid1, Moustafa Mohamad1
Search and Discovery Article #10351 (2011)
Posted August 22, 2011
*Adapted from oral presentation at AAPG Annual Convention and Exhibition, Houston, Texas, USA, April 10-13, 2011. 1Qarun Petroleum Company, Cairo, Egypt. ([email protected])
Abstract The Beni Suef Basin is a relatively under-explored basin in N. Central Egypt. It lies approximately 150 km south of Cairo and is bisected by the present day Nile Valley. It is currently believed that hydrocarbons, sourced from the Albian Lower Kharita (shales and siltstones) and Turonian Abu Roash F (carbonates), have been expelled and have subsequently migrated into up-dip structural closures along the margins of the basin. The stratigraphic column of the Beni Suef Basin extends from the Pre-Cambrian granitic basement through the major Cretaceous reservoirs and seals and up into the Eocene Apollonia carbonates. Late Tertiary to recent deposition is also recorded within the ancestral Nile valley and along its margins. Some uncertainty exists as to the age of inception of the Beni Suef Basin and the extent of sedimentation within the basin prior to the deposition of the Lower Kharita shales. Current 3D seismic mapping is endeavoring to delineate more clearly these older sedimentary packages. The Beni Suef Oil Field was discovered in September 1997 by Seagull Energy Corporation and was followed by the discovery of five additional oil fields - Azhar, Yusif, Gharibon, Lahun and Sobha by Qarun Petroleum Company. Beni Suef Oil Field contains excellent reservoir quality rocks in both the Kharita and Bahariya Formations with additional reserves being calculated in the Abu Roash "A & G" Members. Due to some of the complex mineralogy observed in the Cenomanian Bahariya Formation a detailed petrophysical model was built using Schlumberger’s ELAN&IP software to ensure an accurate understanding of reservoir properties could be achieved. This petrophysical work combined with detailed sedimentological work has greatly aided the understanding of the field’s reserves distribution.
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Recent geochemical work along with detailed mapping of newly acquired 3D seismic is greatly helping the delineation of the two potential source rocks and helping to formulate a clearer picture of hydrocarbon expulsion and migration within the Beni Suef basin. The results of this work may be applicable to the hydrocarbon potential of other basins such as the Minya and Asyut basins of Upper Egypt.
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Qarun Petroleum CompanyQ C p y
Beni Suef Basin
The Key ForThe Key ForExploration Future Success in Upper Egypt
*By
Hemida Zahran * Khaled Abu Elyazid Mostafa Mohamad
April 2011
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AFRICA
EGYPT
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LahunYusif
B. Suef Concession
B S f
AFRICAAzhar
B. Suef
EGYPTGharibonSohba
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Matruh - ShushanBasins
Alamein Basin
Abu El-GharadigBasin
Gindi Basin
Qarun Field
Karama Field
W. Rayan Field
Qarun Field
100 km.0
Basins Distribution Map
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Matruh - ShushanBasins
Alamein Basin
Abu El-GharadigBasin
Gindi Basin
Qarun Field
Karama Field
W. Rayan Field
Qarun Field
B. Suef Basin
100 km.0
Basins Distribution Map
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Stratigraphic Column of B. Suef Basin
R iReservoires :
A / R “ A E & G “
Bahariya & Kharita
A / R A , E & G
Bahariya & Kharita
Source Rocks :A / R “ F “ carbonatesA / R F carbonates
L. Kharita Shale & Siltstone
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2D & 3D Seismic Surveys In Beni-Suef Concession
247 Km(2004)
2
East of NileWest of Nile
598 Km(2009)
2
700 Km (2007)
2
3D : 2429 km2
884 K 2
2D : 3034 km
884 Km(2008)
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Combined TWT Structure maps
East of Nile
West of Nile
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Combined TWT Structure maps
East of Nile
West of Nile
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Lahun
B. Suef
Yusif
Azhar
West Of Nile
Gharibon
SohbaSohba
East Of NileEast Of Nile
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Lahun
B. Suef Yusif
Azhar
West Of Nile
Gharibon
SohbaSohba
East Of NileEast Of Nile
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B. Suef Field Bahariya Depth Structure
N
B. Suef – 1x
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B.Suef – 5x Kharita
O.W.C @ 7100` / - 6890`
= 20-22 % SW =15-20 % NP = 70 ft.
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B. Suef Field A / R “ A “ Depth Structure
N
B. Suef – 11
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BS-11 Abu Roash “A” Pay Sands
3580
3596
3605
36163616
3624
3640
36523658
= 19 % SW =35 % NP = 23 ft.
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Lahun
B. Suef
Yusif
Azhar
West Of Nile
Gharibon
SohbaSohba
East Of NileEast Of Nile
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Azhar Field Bahariya Depth Structure
NAzhar E – 2
Azhar – 1x
Azhar E – 1x
Azhar E – 3
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Azhar – 1x Kharita SandKharita Zone – 1 8148 / - 7623
Kharita Zone – 2 8218 / - 7692
Kharita Zone – 3 8298 / - 7770
O. W. C. 8350 / - 7821
= 14 % SW =38 % NP =80 %
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Azhar E. – 1x U. Bahariya
= 21 % SW =40 % NP = 12 ft.
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Azhar E. – 1x Up. A / R “ G – 5 “
6348
6374
= 12 % SW =32 % NP = 20 ft.
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Y ifLahun
B. Suef
Yusif
Azhar
West Of Nile
Gharibon
SohbaSohba
East Of NileEast Of Nile
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Yusif Field L. A /R “ G “ Depth Structure
NYusif – 4
Yusif 1x
Yusif – 2
Yusif – 1x
Yusif – 3
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Yusif – 1x L. A / R “ G “ Sands
= 17 % SW =48 % NP = 21.5 ft.
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Yusif - 3 U. Bahariya Sands
7150
7170
= 17 % SW =29 % NP = 20 ft.
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Yusif - 4 L. Bahariya Sands
7640
7660
= 14 % SW =50 % NP = 14 ft.
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Lahun
B. Suef
Yusif
Azhar
West Of Nile
Gharibon
SohbaSohba
East Of NileEast Of Nile
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Lahun Field Bahariya Depth Structure
N
Lahun – 1xLahun 1x
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Lahun -1x U. Bahariya
6060
6080
= 15 % SW =32 % NP = 29 ft.
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LahunWest Of Nile
B. Suef
YusifWest Of Nile
Azhar
East Of Nile
GharibonGharibonSohba
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Gharibon Field A / R “ G “ Depth Structure
N
Gharibon – 1x
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Gharibon – 1x A / R “ G – 10 “
7108
7130
= 21 % SW =42 % NP = 16 ft.
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Lahun
B. Suef
Yusif
Azhar
West Of Nile
Gharibon
S hbSohba
East Of NileEast Of Nile
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NW SE
Sohba – 1xNW SE
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Depth Structure Top A / R “E” Sand
NSohba NE 1xSohba NE – 1x
Sohba – 1x
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Sohba – 1x A / R “ E “
7010
7020
O.W.C @ 7032` / - 6354`
= 19 % SW =35 % NP = 23 ft.
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Beni Suef Oils Correlation
Oil-oil correlation for the oils recovered from Beni Suef
Concession suggests there are two oil groups .
Group I : includes the oils that appear to be generated fromincludes the oils that appear to be generated from
predominantly terrestrial organic matter and are
represented by Beni Suef-1X, Azhar -1X and Yusef -1X
oils These oils appear to be generated at a high thermaloils. These oils appear to be generated at a high thermal
maturity ( Paraffinic waxy , high API & high Pour Point . )
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Beni Suef Oils Correlation
Group II :Group II :
represented by Azhar -7X, Azhar E-1X, Sohba -1X and
Gharibon-1X oils appears to be generated from a
predominantly marine organic matter at moderatepredominantly marine organic matter at moderate
thermal maturity ( API 25° , pour point Zero ).
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A : Terrestrial Source
10.00
CB DAB : Peat/Coal SourceC : Mixed SourceD : Marine Source
1.00
n-C
17
Group “II” OilsGroup “I” Oils
Pr/n
0.10
A h E 1X A/R "G" 6348 6374 ftAzhar -7X A/R G5 6325 ft Azhar E-1X A/R "G" 6348-6374 ft
Sohba-1X A/R "E" Sand 7020 ftAzhar-1 Kharita 8146-8164 ft
Yusef-1 L. A/R "G" 6565-6610 ft Gharibon-1 A/R "G" 7108-7130 ftBeni Suef-1 Kharita DST # 3 7033-7075 ft
0.01
0.01 0.10 1.00 10.00
Beni Suef-1 Bahariya DST # 4 6800 ftBeni Suef-1 Bahariya RFT 6869 ft
Plot of Pr/n-C17 vs. Ph/n-C18 for OilsPh/n-C18
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ConclusionsStratigraphic column of E.Desert is similar to W.Desert with the exception that Basin inception may be controlled by Aptian/Albian NE-SW extension and resulted in the Kharita Formation being deposited di tl b tdirectly on basement.
Major part of Beni Suef basin is located in theEast of Nileast o e
Three oil discoveries were achieved based on 2D seismic interpretation and other three oil discoveries
hi d b d 3D i i i t t tiwere achieved based on 3D seismic interpretation .
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Geochemical studies confirmed presence of two oil families in Beni Suef basin, first is generated from lower Kharita shale & siltstones, second is generated from A/R “F”from A/R “F”.
Basement is encountered in Azhar-2 & Azhar-5 more than 12¸000 ft which confirmed the presence of more ¸ pthan 1500 ft of shale & siltstone as an excellent source rock of lower Kharita.
Very high gas readings were recorded (more than 30%)Very high gas readings were recorded (more than 30%) while drilling L. Kharita shale & siltstones in Azhar field which could be a gas producer in future by usingwhich could be a gas producer in future by using hydraulic frac.
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Recommendations
The results of this work may be applied to the south for hydrocarbon potential of other basins such as Minya & Assyut of Upper Egypt.
Conduct required geological studies to evaluate lower Kharita shales & siltstones as gas producerKharita shales & siltstones as gas producer.
Re-evalute any dry hole well data in the light of applying hydraulic frac. and in case of having encouraged results, study the visibility of re-enter or drill a twin well.
Conduct hydraulic frac. in case of having poor oil rate or oil slugs in the testing of an exploratory well .oil slugs in the testing of an exploratory well .
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AcknowledgementAcknowledgement
This contribution reflects work carried out as joint Exploration team between QPC, Dana Petroleum and Apache. All staff involved are acknowledged here for their in put and g pefforts. In closing EGPC, QPC, Dana Petroleum and Apache Egypt managementPetroleum and Apache Egypt management are thanked for their in put and permission to release this informationrelease this information.
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