EGAS. Ministry of Petroleum and Mineral Resources

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2 N. Idku. (A) RWE Rosetta North BG W. Delta Deep Marine Area-5 BG Meret Dev. N. Damietta BALTIM E. IEOC W. ABU MADI IEOC S. Khilala W. Khilala W. Abu Khadra E. Abu Khadra E. Delta Dev. N E. Abu Zahra El. W astani Azhar Delta S. zarka E.El. W astani Dabayaa Luzi dev. Sondos El Burg BG Begonia W.Qantara Area -1 Dev. Qantara Dev. EGAS EGAS CONCESSIONS MAP AND 2015 INTERNATIONAL BID ROUND BLOCKS M E D I T E R R A N E A N Block 6 S. TENNIN OFFSHORE Total area 1275 km 2 Block 7 S E A N. EL HAMMAD OFFSHORE Total area 1927 km 2 Block 8 E. ALEXANDRIA OFFSHORE Block 5 W. EL TEMSAH OFFSHORE Total area 1081 km 2 N. Leil offshore IEOC Block 4 N. RAS EL ESH OFFSHORE Total area 1389 km 2 Block 3 N. ROMMANA OFFSHORE Total area 1882 km 2 Block 2 N E. PORT SAID OFFSHORE W E Total area 1855 km 2 Block 1 Karawan offshore Shorouk N. El Max Offshore N. Tennin Offshore IEOC Offshore N. Port Fouad bp bp IEOC Total area 1749 km 2 offshore EDISON W. EL ARISH OFFSHORE Total area 1797 km 2 S El Salum Matruh El Dabaa ALEX.-2 ( B & B 2 ) bp B2 ALEX.-1 DEV. ( A & A1 ) bp W. Med. -2 DVL bp W. MED. DEEP WATER W. Med-1 bp bp B WDDM -4 BG A1 N. Idku. RWE ( B ) Restricted area Alexandria A Abu Qir (A) Edison Rosetta 8 & 10 BG N. El Amriya RWE Abu Qir (B) Edison WDDM -2 BG W. Delta Deep Marine BG 8 WEB South Dev. N. El Amriya RWE S.Idku Onshore Petrocaltic WDDM -8 BG Rosetta West BG Rosetta Dev. BG W. Delta Deep Marine Area-3 BG Rhamat D. L. Aten dev. 7 WDDM -7 BG DISOUQ AREA-1 DEV. WDDM -6 BG N. E. BALTIM IEOC bp BALTIM N. IEOC BALTIM S. IEOC NW. Khilala W. ABU MADI IEOC T1 Tennin Dev. IEOC N. Damietta Offshore bp Satis Dev. bp Abu Madi EGPC S. El.Mansoura Dev. 6 El Matariya BP N. Gamasa DV. BG Balsam N. Damietta Offshore bp 5 Taurt North bp Seth &Ha py Dev. bp Seth South bp El Burg BG Denise 4 El Temsah IEOC El Temsah Karous W.El Manzala El Basant Area -1 Ashtom Dev. S. Abu Elnaga El Gamil W. Dikirnis E. Dikirnis El Qantara Melrose 2 N. El salhiya onshore W. Qantara DANA GAS El Tamad Sama Area-1 Dev. Dev. N. El Mahala onshore TOTAL 1 N. Tineh Offshore (b) Bp N. Port Said IEOC Restricted area Port said N. Tineh Offshore (a) Bp N. Bardawil Dev. 3 2 N. Thekah offshore Edison Rose Dev. Tao/ Kamose PERINCO Thekah Dev. 1 N.El Arish Offshore Dana Gas El Arish Western Desert S. Disouq Onshore Sea Dragon 30 Sinai 26 EGAS Agreements EGAS Development leases 12 Agreements Under EGAS Supervision Bid Round 2015 EGPC Development leases Restricted areas Offshore open areas Onshore open areas

3 EGAS 2015 International Bid Round comprises eight (8) exploration blocks, offered for competitive bidders under Production Sharing Agreement (PSA). Introduction The 8 offered blocks are all located offshore in shallow to moderate water depths less than 550m, in the Mediterranean Sea region lying between the Abu Qir Bay and El Arish city, with areal extents ranging between 1081 km 2 and 1927 km 2. The offered blocks are present in close proximity to the three major trends of gas-condensate fields: The NW-SE Temsah-Akhen Trend (e.g., Ha py, Akhen, Temsah, Wakar, Port Fouad Marine PFM, etc...); The NNW-SSE Abu Madi Trend (e.g., Baltim North, Baltim East, Baltim South, Abu Madi, etc ); and the NE-SW Rosetta Trend (e.g. Sienna, Simian, Saphire, Taurus, etc ). The fields of these trends comprise combination structural/stratigraphic traps involving sandstone reservoirs of Pliocene and/or Miocene age. Ruby Raven Fayoum Libra Taurus Saurus Saphire Offered Blocks Saffron Scarab Serpent Simian Sienna Rashid N Development Lease Area Taalab Tennin Tennin W Baltim NE2 Baltim NE1 Baltim N Baltim E Baltim S Nidoco Abu Madi Ringa TaurtDenise N H apy Akhen Tuna Seth Temsah Seti-Plio Barboni Mayas Asfour Segan Zaraf Assad Abu Seif Wakar 5 Gas Fields/Discoveries Semman Gas-Condensate Fields/Discoveries Nouras Tao Karous Darfeel PFM 4 Kamose Thekah Gas Pipeline 1 Condensate Pipeline Oil Pipeline It is also worth mentioning that some oil occurrences have been discovered in the eastern area of the offered blocks. These oil occurrences comprise the Mango-1 sub-commercial oil discovery (drilled by Total in 1985 and tested BOPD from the Lower Cretaceous sandstones) and the Tineh-1 subcommercial oil discovery (drilled by IEOC in 1981 and tested with light oil recovery from the sandstones of the Oligocene). In addition to these oil occurrences, the area of the offered blocks includes some recent Oligocene gas-condensate accumulations with commercial value (e.g. Satis & Notus). The 8 offered blocks are situated in an area with well-established infrastructure for gas-condensate production/transportation, connecting the offshore producing fields with the onshore terminals.

4 Nile Delta Basin & Offshore North Sinai - Regional Framework The eight (8) offered blocks are all situated in the Nile Delta Basin, except for Block 1 which lies Offshore North Sinai, at the eastern periphery of the basin with the Pelusium Line crossing the southern part of the block. The Pelusium Line comprises a NE-SW shear lineament separating the Sinai Plate to the south from the Levant Plate to the north Offshore North Sinai occupies the 3 southeastern Mediterranean region and constitutes the southern part of the Levant Plate. It comprises the northern extension of Offered Blocks Gas Fields/Discoveries Major Fault Trends the Syrian Arc inversion Development Lease Area Gas-Condensate Fields/Discoveries Minor Faults structures; such structures comprise large buried inversion anticlines initiated in the Late Mesozoic and continued slightly during the Cenozoic, and formed NE-trending asymmetrical folds. One of these buried anticlinal structures, located to the east of Block 1, was drilled by the Mango-1 well in The well was tested and flowed oil at a rate of BOPD from the Lower Cretaceous sandstones. However, after appraisal drilling, Total decided not to develop the discovery due to sub-commerciality. Despite being of sub-commercial value, the well results indicate the presence of a working hydrocarbon system with oil generation in the area.

5 The Nile Delta Basin is mainly a gas and condensate province with numerous fields made up of combination structural /stratigraphic traps involving sandstone reservoirs of Pliocene and/or Miocene age. Some oil occurrences have also been found in the basin and recent offshore drilling operations are mainly targeting the deeper Oligocene section. Such drilling operations resulted in a number of yet to be developed gas-condensate finds with substantial hydrocarbon resources in sandstone reservoirs of Oligocene age. The Nile Delta Basin straddles the present day Mediterranean shoreline and embraces the farmed lands of the onshore Nile Delta in its southern part and extends offshore till latitude N. About 70% of its areal extent lies offshore in water depths up to 2800 m. The basin overlies the passive margin of northeast Africa with depth to basement reaching 9 to 10 km. The onshore sector of the Nile Delta Basin is crossed by an E-W striking narrow zone (Hinge Zone) of down-to-the-north rotated fault blocks. This zone marks the transition from thick, normal continental crust in the south, to extended continental crust under both the northern onshore Delta and (probably) the entire offshore sector of the basin. The southwestern part of the Nile Delta Basin overlies the eastern extension of the Northern Egypt Basin, while its southeastern portion overlies part of the Syrian Arc province. The offshore sector of the Nile Delta Basin comprises two principal structural trends; the NE-SW Qattara-Eratosthenes (Rosetta) Fault Trend and the NW-SE Misfaq-Bardawil (Temsah) Fault Trend. The Rosetta Fault Trend forms part of a longer fault system extending from the Qattara Depression (southwest of the Nile Delta) to the Eratosthenes Seamount at the northeast corner of the basin. The Misfaq-Bardawil trend is the most obvious expression of the NW-SE trend, which was active later, in the Pliocene, in a strike-slip sense, triggering salt movement and controlling sedimentation patterns. These two major fault trends, the Rosetta and Temsah, are controlling the distribution of significant gas-condensate fields and discoveries (e.g. the Rosetta and Temsah trends of gas-condensate fields/discoveries). In addition to the three major fault trends (the E-W trend of the Hinge Zone, the NE-SW Rosetta Trend and the NW-SE Temsah Trend), the Nile Delta Basin comprises a NNW-SSE Trend known as the Gulf of Suez (GOS) Trend. This fault trend is controlling the distribution of the Abu Madi Trend of gas-condensate fields. Nile Delta Basin & Offshore North Sinai - Regional Framework (continued) Herodotus Basin Qattara Ridge Nile Coastal/Deep Water Sub-Basin (Nile Delta Basin) Alamein Sub Basin- Nile Delta Basin Nile Delta Basin Kattaniya-Qantara High (Syrian Arc) Syrian Arc Levantine Deep Marine Basin

6 Nile Delta Basin - Generalized Stratigraphic Column The nature of the basement beneath the sedimentary succession of the Nile Delta Basin is almost entirely unknown. The prospective section starts with Mesozoic strata (including potential source rocks) at the base, probably resting on crystalline basement. The Mesozoic succession represents a rifted passive margin, formed at the opening of the Neo-Tethys Ocean in the Late Triassic to Early Jurassic. Late Cretaceous to Early Tertiary dextral transpression generated the NE-SW trending structures of the Syrian Arc system. Passive margin sedimentation, mainly clastics but with some platform carbonates in the Eocene, continued through the Paleogene. Sedimentation rates increased in the Late Oligocene or Early Miocene, with northward tilting associated with opening of the Red Sea and Gulf of Suez to the south. Outbuilding of coastal and deltaic sediments was interrupted by the Mediterranean-wide sea level lowering in the Messinian (latest Miocene), when a deep and extensive canyon system was incised into the earlier strata. Filling of the canyon with fluvial sands of the Abu Madi Formation took place as base levels rose again at the end of the Miocene. Evaporites were deposited at about the same time, to seaward; they include several kilometers thickness of salt in the deep water sector of the basin, and thin anhydrites nearer to shore. Plio-Pleistocene outbuilding of the delta resumed, towards its present-day configuration. Offshore environments included slope channels that conducted large volumes of reservoir-quality sands away from the shelf into deeper water fan systems.

7 Nile Delta Basin Source Rocks Simian Sienna Taalab Taurus Ruby Raven Fayoum Saffron Serpent Saurus Scarab Saphire Rashid N Libra 8 7 Tennin WTennin Baltim NE2 Baltim NE1 Baltim N Baltim E Baltim S 6 Nidoco Abu Madi 5 Ringa H apy Taurt Denise N Tuna Akhen Seth Seti-Plio Temsah Segan Barboni Asfour Zaraf Abu Seif Wakar Assad Mayas Semman Karous Nouras Darfeel Tao PFM Kamose 4 2 Thekah 1 3 Offered Blocks Development Lease Area Gas Fields/Discoveries Gas-Condensate Fields/Discoveries Extension Of Main Gas Window Extension Of Early Gas Window Extension Of Proven Thermogenic Domain (Pre-Mess. & Mess. Targets) The Nile Delta Basin is a gas and condensate province, with only small amounts of oil. The youngest (Plio-Pleistocene) accumulations are of dry gas only; proportions of condensate (and minor oil) increase with the age of the reservoir. This has led to speculation that at least some of the gas may be of biogenic origin, generated from the Pliocene Kafr El Sheikh Formation. This is partly supported by analytical data, though another possibility is that the gas has been derived by some kind of fractionation process (possibly biologicallymediated) from deeper accumulations. Whether or not this is so, there is also evidence that Oligocene and Lower Miocene shales have sourced some of the basin's hydrocarbons, probably reaching thermal maturity in the Pliocene. Jurassic and Cretaceous source rocks, as in the Northern Egypt Basin, are also likely to have contributed, though the evidence is less direct.

8 MIOCENE EGAS Nile Delta Basin Reservoirs & Seals Proven reservoirs, with known accumulations, extend from Oligocene to Pleistocene in age; all are sands or sandstones. Pliocene reservoirs (Kafr El Sheikh and El Wastani formations) have recently proved to be exceptionally prolific and of very high quality; they include slope-channel sands and deep water fan sands. Upper Miocene reservoirs of the Abu Madi and Qawasim formations are mainly fluvial and were formed in the incised valley system of the Messinian sea level lowstand. The Middle to Upper Miocene Sidi Salim Formation includes good quality sands at several levels, notably near the top (the Wakar Member); sands formed in a range of environments from distributary channels to slope channels and fan-delta. The Lower to Middle Miocene Qantara Formation has recently been shown also to be potentially important, with the Raven 1 discovery; the sands are of shallow marine origin. Seals in the basin are mainly shales, and predominantly intraformational. Upper Miocene (Messinian) anhydrite (Rosetta Member) forms the seal in only a very small number of cases, but the equivalent thick halites may prove to be important as seals in the further offshore sector of the basin. Age Pleistocene PLIOCENE Oligocene Eocene Depth Range of Discovered Reservoirs Lithology Reservoirs Depth Shallow Reservoirs From mt Intermediate Reservoirs > mt Deep Reservoirs HPHT > mt Gas Discovery Reservoir Rock

9 Nile Delta Basin - Plays Approximately 75% of known reserves have been found in combination traps, with both stratigraphic and structural elements. Channelized sands, intraformationally encased in and sealed by shales, typically form the stratigraphic element, whether the deposit is fluvial (as in the Messinian Abu Madi Formation) or of slope-channel or fan delta origin (as in the Pliocene Kafr El Sheikh Formation). The structural element is generally either one or more sealing faults (including growth faults), or a structural culmination over which the reservoir is draped.

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11 Block Summary Block 1: West El Arish Offshore Location: West El Arish Offshore Block is located at approximately 34 km to the west of El Arish City and some 85 km to the east of Port Said City. It is situated directly to the north of Lake Bardawil with the Mediterranean shoreline forming its southern boundary. The block extends northward for approximately 70 km, attaining a maximum water depth of 550 m. The block is situated in an area with wellestablished infrastructure for gas-condensate production / transportation. Total Area: 1797 Km 2 1 Block 1-50 m Water Depth: m Previous Concessionaire: BP & IEOC/ THARWA Nearby Fields & Discoveries : West El Arish Offshore Block is located at approximately 21 km to the west of the Lower Cretaceous Mango-1 oil discovery and about 12.5 km to the east of the Pliocene Thekah gas field.

12 Block Coordinates & Drilled Wells Block 1: West El Arish Offshore Block 1 West El Arish Offshore NO. Lat Long Intersection of Long with Shore Line Intersection of Long with Shore Line Well Name/ Company Spud Date/ Compl. Date TD/ TD Lat./ Long Status NS 21-1 BP 02-Oct Jan M L. Cretaceous 31 25' ' " P&A Dry Hole

13 2D & 3D Seismic Coverage Block 1: West El Arish Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines BG BPNs NS NSI BP_ND1& Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) Thekah 1404 Thekah Nargis 679

14 Block 1 Prospectivity Examples Block 1: West El Arish Offshore West El Arish Offshore Block is located Offshore North Sinai, at the eastern periphery of the Nile Delta Basin. The block is crossed, in its southern part, by the Pelusium Line. This line comprises a NE-SW shear lineament separating the Sinai Plate (onshore) to the south from the Levant Plate to the north. Offshore North Sinai constitutes the southern part of the Levant Plate and comprises the northern extension of the Syrian Arc inversion structures. These inversion structures comprise large buried anticlines initiated in the Late Mesozoic and continued slightly during the Cenozoic, and formed NE-trending asymmetrical folds. West El Arish Offshore Block is located at approximately 21 km to the west of the Lower Cretaceous Mango-1 oil discovery and about 12.5 km to the east of the Pliocene Thekah gas field. It also lies to the east of the Oligocene Tineh-1 oil discovery Pliocene Play Concept: A B Source: Reservoir: Massive shales of Kafr El Sheikh Fm. Mainly represented by massive to laminated Seal: Trapping: sands, lying up dip within a growth faulted block of Kafr El SheikhFm. Massive shales of deep marine deposits provide the top and lateral seal for the target reservoirs. Combined structural/stratigraphic traps created/associated to listric growth faults. A B

15 EGAS Block 1: West El Arish Offshore Cretaceous and Oligo/Miocene Play Concept: Top Cretaceous 4-way dip closure NW SE NW Source: The Late Jurassic carbonate and the Oligocene shale of the Tineh fm. SE K1 prospect Reservoir: Sandstones of the Lower Cretaceous & Oligo/Miocene. Seal: Top seal is provided by intra-formational shales and lateral seal is attained through sand-shale juxtaposition along sealing faults. Trapping: Structural trap related to compressional phase of the Syrian arc system.

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17 Block Summary Block 2: East Port Said Offshore Location: East Port Said Offshore Block is located at approximately 98 km to the WNW of El Arish City and some 72 km to the northeast of Port Said City. The southern boundary of the block is situated some 32 km to the north of the Mediterranean shoreline with its northern boundary extending for additional 45 km. The block is situated in an area with well-established infrastructure for gascondensate production/transportation. Total Area: 1855 Km 2 Water Depth: Ranges from 20 m to 350 m 2 Block 2-50 m Previous Concessionaire: BG & IEOC Nearby Fields & Discoveries : East Port Said Offshore Block lies to the east of numerous fields of the Temsah-Akhen Trend with gas-condensate production, mainly from Miocene sandstone reservoirs. The block encompasses three development lease areas (Tao, Kamose & North Bardawil) of the Tao, Kamose and Zaraf gascondensate fields respectively.

18 Block Coordinates & Drilled Wells Block 2: East Port Said Offshore Block-2 East Port Said Offshore NO. Lat Long Kamose Development Lease No. Latitude Longitude Tao Development Lease No. Latitude Longitude North Bardawil Development Lease No. Latitude Longitude Tao Dev Kamose Dev Well Name/ Company Spud Date/ Compl. Date TD/ TD Lat./ Long Status Assad-1 DIR 05-Oct M 31 45' IEOC 08-Nov-02 K. El Sheikh (Pliocene) 32 44' " T&A Gas Discovery Hadil-1 ST 25-Jul M 31 42' IEOC 29-Aug-05 K. El Sheikh (Pliocene) 32 49' " P&A (Pliocene Gas Samples) Nardine-1 16-Nov M 31 39' IEOC 26-Jan-09 Sidi Salem (Miocene) 32 40' 35.78" T&A Gas Shows Seridia-1 12-Apr M 31 24' IEOC 5-May-10 K. El Sheikh (Pliocene) 32 48' 35.57" T&A Gas Discovery

19 2D & 3D Seismic Coverage Block 2: East Port Said Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines NS S_Lines 86 8 BP_ND 1& TGS & Veritas 49 3 NS NSI Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) Thekah 1272 Tineh 717 N.Bardawil 433

20 Block 2 Prospectivity Examples Block 2: East Port Said Offshore East Port Said Offshore Block is located in the Eastern Nile Delta Offshore area, at the southeastern end of the NW-SE Temsah-Akhen Trend of gas-condensate fields. The fields of this trend comprise stratigraphic/structural combination traps involving Pliocene and Miocene sandstone reservoirs aligned along the NW-SE Misfaq- Bardawil Temsah fault. The three development leases (Tao, Kamose & North Bardawil) situated within the perimeter of the block, constitute the southeastern extension of the Temsah Trend with dry gas production from clastic sandstone reservoirs of Plio-Pleistocene age. In addition to its proximity to the numerous gas-condensate fields of the Temsah Trend, the block is also situated to the north of the Tineh-1 Oligocene oil discovery. In addition to its location in the above mentioned setting, East Port Said Offshore contains two gas discoveries (Assad-1 Dir. in the northern part of the block and Seridia-1 in the southern part) in the sandstones of the Plio-Pliestocene section. The Assad discovery was developed and depleted, while the Seridia discovery is yet to be appraised/developed. Pliocene Play Concept: Source: Reservoir: Massive shales of Kafr El Sheikh Fm. Mainly represented by massive to laminated sands, lying up dip within a growth faulted block of Kafr El Sheikh Fm. Seal: Massive shales of deep marine deposits provide the top and lateral seal for the target reservoirs. Trapping: Combined structural/stratigraphic traps formed by channel fill features within roll over anticlinal structures created/associated to listric growth faults.

21 Block 2: East Port Said Offshore Messinian Play Concept: S N Source: The shales of the Oligocene Tineh fm and the Early Miocene Qantara fm. Reservoir: Sandstones of the Upper Miocene Tortonian Wakar formation. These sandstones are anticipated to rich gas potential. Seal: Top seal is provided by the overlying Messinian salt, while lateral seal is essentially by intra-formational shales. Trapping: Anticlinal feature with 4-way dip closure.

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23 Location: Block Summary Block 3: North Rommana Offshore North Rommana Offshore Block is located at approximately 97 km to the west of El Arish City and some 50 km to the east of Port Said City. It is situated directly to the north of Lake Bardawil with the Mediterranean shoreline forming its southern boundary. The block extends northward for approximately 36 km, attaining a maximum water depth of 20 m. The block is situated in an area with well-established infrastructure for gas-condensate production/transportation. Block 3 Total Area: 1882 Km 2 Water Depth: 0-20 m Previous Concessionaire: Conoco, Phillips & IEOC Nearby Fields & Discoveries : North Rommana Offshore Block lies to the southeast of numerous fields of the Temsah-Akhen Trend with gascondensate production, mainly from Miocene sandstone reservoirs. It also lies to the south of the three development lease areas of the Tao, Kamose and Thekah gas-condensate fields m

24 Block Coordinates & Drilled Wells Block 3: North Rommana Offshore Block 3 North Rommana Offshore NO. Latitude Longitude º º Intersection of Long. 33º with Shore Line Intersection of Long. 32º with Shore Line 33º º º º º º º º Well Name/ Company Spud Date/ Compl. Date TD/ TD Lat./ Long Status Tineh-1 06-Apr M 31 19' 12.06" IEOC 04-Oct-81 Massajid (Jurassic) 32 48' 02.74" T&A Gas & Condensate Discovery Tineh-2 02-Jun M 31 17' 9.772" IEOC 10-Sep-83 Cretaceous 32 48' " P&A Dry Hole Hout-1 18-Mar M 31 22' " Phillips 15-Aug-93 Early Miocene 32 36' " P&A Dry Hole Bougaz E-1 19-Mar M 31 10' 36.51" IEOC 20-Apr-97 Tineh 32 48' 31.28" T&A Oil Discovery El Fayrouz NE-1 09-Jul M 31 8' " IEOC 7-Aug-00 Tineh (Oligocene) 32 43' " P&A Dry Hole Jd Dec M 31 20' " IEOC 28-Jan-09 K. El Sheikh (Pliocene) 32 58' " P&A Non-Commercial Mesk-1 05-Apr M 31 21' 47.64" IEOC 18-Apr-09 K. El Sheikh (Pliocene) 32 39' 31.98" P&A Dry Hole

25 2D & 3D Seismic Coverage Block 3: North Rommana Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines CMB CMB NS NSI NS S_Lines Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) Thekah OBC 1220 Boughaz 153

26 Block 3 Prospectivity Examples Block 3: North Rommana Offshore North Rommana Offshore Block is located in the southeastern portion of the offshore part of the Nile Delta Basin. The block straddles the southern end of the NW-SE Misfaq-Bardawil (Temsah) fault. The northeastern part of the block lies in the Eastern Nile Delta Offshore area, on trend with the Temsah Trend of gas-condensate fields. The fields of this trend comprise stratigraphic/structural combination traps with mainly Miocene sandstone reservoirs. The southwestern part of the block lies in the Central Nile Delta Offshore area. North Rommana Offshore Block comprises, in its northern part, the Oligocene Tineh-1 discovery. It also lies to the south of the Tao and Kamose gas fields, mainly Pliocene. Cretaceous and Oligo/Miocene Play Concept: Source: The Late Jurassic carbonates and the Oligocene shales of the Tineh fm. Reservoir: Sandstones of the Lower Cretaceous and Oligo/Miocene. Seal: Top seal is provided by intra-formational shales and lateral seal is attained through sand-shale juxtaposition along sealing faults. A A Trapping: The trap is formed by 4-way dip structural closure. A A

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28 Block Summary Block 4: North Ras El Esh Offshore Location: North Ras El Esh Offshore Block is located in the shallow waters of the Mediterranean Sea, at the outlet of Damietta Branch of the River Nile. The southern boundary of the block is formed by the Mediterranean shoreline with its southeastern corner lying directly to the northwest of Port Said city. The northern boundary of the block extends sea-ward for additional km attaining a maximum water depth of 30 m. The block is situated in an area with well-established infrastructure for gascondensate production/transportation. Block 4 Total Area: 1389 Km 2 Water Depth: 0-30 m 4 Previous Concessionaire: Mobil & BG Nearby Fields & Discoveries: North Ras El Esh Offshore Block lies to the southwest of numerous fields of the Temsah-Akhen Trend with gas-condensate production, mainly from Miocene sandstone reservoirs. This is in addition to BG s Abu Madi Harmattan Deep gas-condensate discovery, at the southern boundary of the block, and the Oligocene Notus-1 gas-condensate discovery, located to the north of the western part of the block. Two development lease proposals for the Harmattan and Notus discoveries were submitted to EGAS by BG.

29 Block 4 North Ras El Esh Offshore NO. Lat Long Intersection of Long with Shore Line Intersection of Long with Shore Line Intersection of Long with Shore Line Intersection of Long with Shore Line Block Coordinates & Drilled Wells Block 4: North Ras El Esh Offshore Well Name/ Company Spud Date/ Compl. Date TD/ TD Lat./ Long Status Damietta-1 23-Aug M 31 36' ' Mobil 12-Sep-75 M. Miocene 32 05' '' P&A Dry Hole Je 72-1 ST1 21-May M 31 29' BG 25-Sep-08 Sidi Salem (Miocene) 32 06' " P&A Dry Hole El Burg-1 09-Jun M 31 31' BG 07-Aug-08 Wakar (Miocene) 31 40' " P&A Dry Hole Zonda-1 20-Aug M 31 26' BG 12-Sep-11 K. El Sheikh (Pliocene) 32 06' " P&A Dry Hole

30 2D & 3D Seismic Coverage Block 4: North Ras El Esh Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines Bp_NDD 1& GND 11 1 Others Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) El Burg OBC East 520 El Manzala OBC 651

31 Block 4 Prospectivity Examples Block 4: North Ras El Esh Offshore North Ras El Esh Offshore Block is located in the southeastern part of the Central Nile Delta Offshore area. The northeastern border of the block lies directly to the west of the NW-SE Misfaq-Bardawil (Temsah) fault which hosts to the east, along its trend, numerous gas-condensate fields with stratigraphic/structural combination traps involving Pliocene and Miocene sandstone reservoirs. The block is situated at approximately 30 km to the east of the NNW-SSE Abu Madi Trend of gas-condensate fields which comprise stratigraphic/structural traps, mainly with Miocene sandstone reservoirs. North Ras El Esh Block also lies between BG s recent gas-condensate discoveries of the Abu Madi Harmattan Deep (to the south) and the Oligocene Notus-1 (to the north). Pliocene Play Concept: S N Source: Massive shales of Kafr El Sheikh Fm. Reservoir: Mainly represented by massive to Seal: laminated sands of Kafr El Sheikh Fm. Intra-formational shales of Kafr El N Sheikh Fm. Trapping: Combined structural / stratigraphic trap. S

32 Messinian Play Concept: SSW Block 4: North Ras El Esh Offshore NNE Source: Several source rock UNITS are Reservoir: Seal: anticipated within the Lower Miocene, Oligocene and possibly upper Cretaceous and Jurassic Channel and sheet sands of outer shelf to slope environments. Top seal is provided by intra- Top Mess Intra Tort top Sidi Salem intra Sidi Salem Sidi Salem Deep1 S 1 S 2 S 3 dep th Base Mess evap formational shales and lateral seal is Sidi Salem Deep2 attained through sand-shale Top Qantara juxtaposition along sealing faults. Trapping: 3-way dip closure against NW-SE Trending normal faults. E prospect strike line showing sheet-like fan feature

33 Block 4: North Ras El Esh Offshore Oligocene Play Concept: Source: The Oligocene shale is expected to be the dominant source (self sourcing) in addition to migration from the Mesozoic, Jurassic to Cretaceous which is O1 O2 anticipated through proximal deep seated faults. Reservoir: Seal: Oligocene sand channels within Tineh Fm. The top and lateral sealing lithologies are essentially provided by the intraformational shales. Trapping: Combined structural stratigraphic trap.

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35 Block Summary Block 5: West El Temsah Offshore Location: West El Temsah Offshore Block is located at approximately 56 km to the north of Damietta city and some 93 km to the northwest of Port Said city. The southern boundary of the block is situated about 35 km to the north of Damietta city with its northern boundary extending northward for additional 30 km. West El Temsah Offshore Block lies in water depths ranging between 30 m and 500 m. The block is situated in an area with well-established infrastructure for gas-condensate production /transportation. Total Area: 1081 Km 2 5 Block 5 Water Depth: Ranges between 30 m and 500 m Previous Concessionaire : BP Nearby Fields & Discoveries: West El Temsah Offshore Block lies to the west/northwest of numerous fields of the Temsah-Akhen Trend with gas-condensate production, mainly from Miocene sandstone reservoirs. This is in addition to BG s Oligocene Notus-1 gas discovery, located to the south of the western part of the block; a development lease proposal for this discovery was submitted by BG to EGAS. Wells: No wells drilled yet within the bounds of the block

36 Block Coordinates Block 5: West El Temsah Offshore Block 5 West El Temsah Offshore NO. Lat Long

37 2D & 3D Seismic Coverage Block 5: West El Temsah Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines GND EGP 15 2 BP_NDD 1& TGS & Veritas 27 1 Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) Tennin-Satis 899

38 Block 5 Prospectivity Examples Block 5: West Ministry El Temsah of Petroleum Offshore Block 5: West El Temsah Offshore West El Temsah Offshore Block is mainly located in the eastern part of the Central Nile Delta Offshore area, with only small portions (its northeastern parts) lying in the western part of the Eastern Nile Delta Offshore area. The block straddles the NW-SE Misfaq-Bardawil (Temsah) fault with its northeastern portion lying at the northwestern end of the numerous gas-condensate fields of the Temsah Trend aligned along this fault. Such fields of this trend comprise stratigraphic/structural combination traps involving Pliocene and Miocene sandstone reservoirs. West El Temsah block is situated at approximately 40 km to the east of the NNW-SSE Abu Madi Trend of gas-condensate fields which comprise stratigraphic/structural traps, mainly with Miocene sandstone reservoirs. The block also lies to the north of BG s Oligocene Notus-1 gas-condensate discovery. Pliocene Play Concept: A A Source: Massive shales of Kafr El Sheikh. Reservoir: Mainly represented by massive to laminated sands of Kafr El Sheikh Fm. Seal: The top and lateral seal is provided by Kafr Trapping: El Sheikh massive shales. Combined structural stratigraphic trap. A A Possible Target ( Pliocene ) Inline no

39 Block 5: West El Temsah Offshore Oligocene Play Concept: NW SE Source: The Oligocene shale is expected to be the Reservoir: dominant source (self sourcing) in addition to migration from the Mesozoic, Jurassic to Cretaceous which is anticipated through proximal deep seated faults. Oligocene sand channels within Tineh Fm O6 RMS amplitude and Miocene sands where vertical communication may accur through deep NW U O2 seated faults U. O3 Seal: Intra-formational shales of the Oligocene are L. O3 O4 anticipated to provide the top and lateral seal O5 Trapping: for the prospect. Combined structural stratigraphic trap. SE Well location 3km O6 Depth Map

40 EGAS

41 Block Summary Block 6: South Tennin Offshore Location: South Tennin Offshore Block is located at approximately 97 km to the northwest of Port Said city and some 151 km to the northeast of Alexandria city, with the Mediterranean shoreline forming its southern boundary. The block extends seaward for additional 64 km attaining a maximum water depth of 250 m. South Tennin Offshore Block is situated in an area with well-established infrastructure for gascondensate production /transportation. Total Area: 1275 Km 2 Block 6 6 Water Depth: m Previous Concessionaire: IEOC, Amoco, Shell & BG Nearby Fields & Discoveries: South Tennin Offshore Block is located directly to the east of the Abu Madi Trend of gas-condensate fields (Baltim East, Baltim North, Baltim South, etc..), producing from Miocene sandstone reservoirs. This is in addition to BG s Oligocene Notus-1 gas-condensate discovery, located to the east of the central part of the block; a development lease proposal for this discovery was submitted by BG to EGAS.

42 Block 6 South Tennin Offshore NO. Lat Long Intersection of Long with Shore Line Intersection of Long with Shore Line Block Coordinates & Drilled Wells NO. Lat Long Block 6: South Tennin Offshore Well Name/Company Spud Date/Compl. Date TD Lat./Long Status Nidoco M-1 IEOC Sekhmet-1 Amoco Sekhmet-2 Amoco Jg 66-1A (Aida-1) Shell JF 65-1 Shell Jh 64-1 Shell Opera Offshore-1 BG 14-Aug Sep Aug Oct Mar-95 9-Apr Mar-01 2-Jun Apr May-06 1-Nov Dec Feb-14 4-Apr M Qawasim (Miocene) 3358 M Sidi Salem (Miocene) 3380 M Sidi Salem (Miocene) 3770 M Sidi Salem (Miocene) 3412 M Qawasim (Miocene) 5760 M Tineh 1950 M K. El Sheikh (Pliocene) 31 37' ' " 31 39' ' 28.29" 31 42' ' " 31 40' ' " 31 35' ' " 31 46' ' " 31 43' ' " P&A Dry Hole P&A Dry Hole P&A Dry Hole P&A Dry Hole P&A Dry Hole T&A Gas discovery (non-commercial) T&A Gas discovery (non-commercial)

43 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines EGP 28 2 GND Bp_ND1& Others 84 9 Total D & 3D Seismic Coverage Block 6: South Tennin Offshore 3D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) NGO El Burg OBC West 158 Tennin-Satis 735 NWD 977

44 TWT ms EGAS Block 6 Prospectivity Examples Block 6: South Tennin Offshore South Tennin Offshore Block is located in the southern part of the Central Nile Delta Offshore area, directly to the east of the NNW-SSE Abu Madi Trend of gascondensate fields (e.g. Baltim N, Baltim E, Baltim S & Nidoco) which comprise stratigraphic/structural traps, mainly with Miocene sandstone reservoirs. The block is also situated to the west of the recent Oligocene Notus-1 gas-condensate discovery and embraces the Satis Development Lease in its northern part. In addition to that, two wells (Opera Offshore-1 and Jh 64-1) out of the 7 wells drilled in the block recorded gas shows in the sandstones of the Pliocene section. Pliocene Play Concept: Source: Massive shales of Kafr El Sheikh. N 500 Plio 70 S Reservoir: Seal: Sandstone slope channels within the Upper Pliocene. The massive shale of deep marine P 1 top KES deposits provides the main seal. This shale forms both top and lateral 2000 seal for the target reservoirs. Trapping: The trapping mechanism is mainly 2500 stratigraphic 5km

45 Block 6: South Tennin Offshore Oligocene Play Concept: S N Source: Oligocene source rock is the main hydrocarbon generator anticipated for the play. Reservoir: Oligocene reservoir is expected to be developed mainly in slope channel turbidities. Seal: Intra-Oligocene shales as well as shale package of expected lower Miocene age (Qantara Fm.) is anticipated to provide the regional top seal. S Trapping: 4-way dip structural closure comprising channel fill stratigraphic features associated with roll over anticlines. N

46 EGAS

47 Block Summary Block 7: North El Hammad Offshore Location: North El Hammad Offshore Block is located at approximately 94 km to the WNW of Damietta City and some 109 km to the ENE of Alexandria City. It is situated directly to the north of Lake El Burullus with the Mediterranean shoreline forming its southern boundary. The northern boundary of the block extends seaward for 49 km attaining a maximum water depth of 250 m. North El Hammad Offshore Block is situated in an area with well-established infrastructure for gas-condensate production/transportation. Block 7 7 Total Area: 1927 Km 2 Water Depth: m Previous Concessionaire : Elf AQ & IEOC Nearby Fields & Discoveries: North El Hammad Offshore Block is located directly to the west of the Abu Madi Trend of gas-condensate fields (Baltim East, Baltim North, Baltim South, etc..), producing from Miocene sandstone reservoirs. It also lies to the east and southeast of the Rosetta Trend of gascondensate fields (Pliocene & Miocene). Additionally, the block encompasses IEOC s Aten Development Lease (proposal) and surrounds bp s Rahamat Development Lease.

48 NO. Lat Long Intersection of Long with Shore Line Intersection of Long with Shore Line Well Name/Company Spud Date/Compl. Date TD Lat./Long Status Baltim-1 IEOC W. Blatim-1 IEOC Block 7 North El Hammad Offshore Aten Development Lease No. Latitude Longitude Sep Dec Jul Oct-07 Block Coordinates & Drilled Wells NO. Lat Long M M. Miocene 4590 M Qantara (Miocene) ' ' 14.05" 31 53' ' " P&A Dry Hole T&A Block 7: North El Hammad Offshore

49 2D & 3D Seismic Coverage Block 7: North El Hammad Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines EGP GND WDD WDN Bp_NDD 1& Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) W. Baltim 1136 SW. Baltim 465 Burullus-Rosetta 725

50 Block 7: North El Hammad Offshore North El Hammad Offshore Block is located in the western part of the Central Nile Delta Offshore area, directly to the southeast of the NE-SW Rosetta Trend of gascondensate fields. The fields of this trend comprise channel sandstones of Pliocene age forming stratigraphic traps, within the surrounding intraformational shales of Kafr El Sheikh, frequently associated with structural component and showing significant amplitude anomalies on seismic sections. Also, the Rosetta Trend includes some fields involving Miocene sandstone reservoirs in stratigraphic/structural combination traps with rich gas potential. North El Hammad Offshore Block is situated to the west of the NNW-SSE Abu Madi Trend of gas-condensate fields (e.g. Baltim N, Baltim E, Baltim S & Nidoco) which comprise stratigraphic/structural traps, mainly with Miocene sandstone reservoirs. In addition to its location in the above mentioned setting, North El Hammad Offshore encompasses IEOC s Pliocene Aten Development Lease (proposal) and surrounds bp s Lower Miocene Rahamat Development Lease. Pliocene Play Concept: Block 7 Prospectivity Examples Source: Reservoir: Massive shales of Kafr El Sheikh Fm. Anticipated to comprise sandstone channel-like features within Kafr El Sheikh Fm. Seal: Provided by intra-formational shales of KES Fm. Trapping: Stratigraphic/structural combination trap. Attribute Map Arbitrary line showing channel extension Arbitrary Line

51 Block 7: North El Hammad Offshore Oligocene Play Concept: Source: Reservoir: Seal: Trapping: The Oligocene shale is expected to constitute the main source (self sourcing) in the area, in addition to anticipated migration from the Mesozoic, Jurassic to Cretaceous source rocks through proximal deep seated faults. Oligocene channel sandstones within the lower part of the Tineh Fm. Intra-formational shales of the Oligocene are anticipated to provide the top and lateral seal. 4-way dip structural closure. Well trajectory

52 EGAS

53 Block Summary Block 8: East Alexandria Offshore Location: East Alexandria Offshore Block is located at approximately 81 km to the northeast of Alexandria City; directly to the northwest of Lake El Burullus. The Mediterranean shoreline forms the southern boundary of the block, while its northern boundary lies seaward at about 64 km in a maximum water depth of 400 m. East Alexandria Offshore Block is situated in an area with well-established infrastructure for gas-condensate production/transportation. Total Area: 1749 Km 2 Block 8 8 Water Depth: m Previous Concessionaire : IEOC, BG Nearby Fields & Discoveries: East Alexandria Offshore Block is bordered from the west and north by the Rosetta Trend of gas-condensate fields (Pliocene & Miocene). Additionally, the block encompasses two established development leases (BG s Rosetta & Roseta West) as well as a development lease proposal by GDF (West El Burullus South).

54 NO. Lat Long Intersection of Long with Shore Line Intersection of Long with Shore Line Block 8 East Alexandria Offshore Rosetta Development Lease (BG) No. Latitude Longitude Block Coordinates & Drilled Wells WEB SOUTH DEVELOPMENT LEASE No. Latitude Longitude Rosetta West Development Lease (BG) No. Latitude Longitude Block 8: East Alexandria Offshore Well Name/Company Spud Date/Compl. Date TD Lat./Long Status Rosetta-2 4-May M 31 37' IEOC 26-Jul-69 M. Miocene 30 22' " P&A Dry Hole NW Rosetta May M 31 44' IEOC 19-Jul-85 Qantara 30 24' " P&A Dry Hole Rosetta-9 4-May M 31 59' Rashpetco 25-May-01 K. El Sheikh (Pliocene) 30 33' " P&A Dry Hole

55 2D & 3D Seismic Coverage Block 8: East Alexandria Offshore 2D Seismic Surveys (Segy Standard Format) Survey Name Line-Km No. of Seismic Lines EGP GND SW 14 1 WDN 10 1 BP_ND1& Total D Seismic Data (Segy Standard Format) Survey Name Area (Sq. Km) Burullus W.Burullus Merge OBC Rosetta98 607

56 Block 8 Prospectivity Examples Block 8: East Alexandria Offshore East Alexandria Offshore Block is mainly located in the southeastern part of the Western Nile Delta Offshore area, with minor portion (its southeastern part) lying in the southwestern part of the Central Nile Delta Offshore area. The block straddles the NE-SW Qattara-Eratosthenes (Rosetta) Fault which hosts along its strike, to the west, numerous gas-condensate fields with mainly Pliocene sandstone reservoirs as well as sandstone reservoirs in the Miocene. Also, the block lies at approximately 25 km to the northeast of the Miocene Abu Qir gas-condensate field. In addition to its location in the above mentioned setting, East Alexandria Offshore Block encompasses three development leases; the BG s Rosetta & Roseta West development leases (in its eastern part) and the GDF s (proposal) of West El Burullus South Development Lease in the southwestern part. Pliocene Play Concept: SE NW Source: Massive shales of Kafr El Sheikh. Reservoir: Mainly represented by massive to laminated sands, lying up dip within a growth faulted block of Kafr El Sheikh Fm. P1 prospect B-package C-package D-package F-package Seal: Intra-formational shales of the Kafr El Sheikh are anticipated to provide the top Seismic amplitude map and lateral seal. Trapping: The combined channel fill stratigraphic features and roll over anticline structures created and associated by listric growth. N

57 RMS Amplitude TWT (ms) EGAS Block 8: East Alexandria Offshore Miocene Play Concept: 2000 Source: Oligocene and early Miocene shales Reservoir: Mainly represented by massive to 2400 laminated sands of slope channel Seal: Intra-formational shales of the Late 2800 Miocene are anticipated to provide the top and lateral seal Trapping: Stratigraphic/structural combination trap T Hig h ABM-U-P1 Prospect 3400 Low 0 km 2 Neg. Seismic Amplitude Post.