SENEGAL BASINS POTENTIAL & ACREAGE By Mrs Nd. Rokhaya.Diallo

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Presentation transcript:

SENEGAL BASINS POTENTIAL & ACREAGE By Mrs Nd. Rokhaya.Diallo Manager Basin Geology Petrosen

Dakar LOCATION AREA : 196 192 Km2 POPULATION : ~12 000 000 hbts DENSITY: 51 h / Km2 GNP : 1110 $ Dakar

overlying a Paleozoic basin REGIONAL SETTING NW African coastal basin the MSGBC Mesozoic-Cenozoic passive margin basin overlying a Paleozoic basin no wells in deep water

RESERVOIRS & SEALS Upper Devonian shales Devonian sandstones :fine to coarse grained, often oolithic with porosities ~ 15% - 20%. Upper Tertiary shaly sequences Lower Tertiary clastics and carbonates Upper Cretaceous sands and shale sequences Jurassic - lower Cretaceous carbonate section Ordovician sandstones : no primary porosity, but intensely fractured, good secondary porosity having excellent deliverabilty

in CM-7 SOURCE ROCKS & MATURATIONc Best source rocks Cenomanian-Turonian and Albian in CM-7 Cenomanian level at 2608m with TOC = 8.72 % HI = 660 mg/g in CM-10 Turonian level at 2554 m with TOC = 5.25 % HI = 638 mg/g

SOURCE ROCKS & MATURATION Silurian shales : best regional source rocks TOC ~ 1% - 3% Ro ~ 0.95 - 1.3

HYDROCARBON OCCURRENCES & PRODUCTIONc F G P Top Neocomian Lmst CRETACEOUS TERTIARY PLIO-RECENT MIOCENE OLIGOCENE EOCENE PALEOCENE CAMPANIAN MAASTRICHT. SANTONIAN TURONIAN CENOMANIAN ALBIAN APTIAN JURA NEOCOMIAN MALM DOGGER 3D SEISMIC PICKING K 130 K 110 K 110 a K 100 K 120 K 090 K 070 T 090 T 060 T 080 T 040 T 030 T 020 MIXED SYSTEMS DELTAIC VS CARBONATE PLATFORM OPEN MARINE CARBONATES Aptian transgression PROGR. CARB. PLATFORM DELTAIC AND SHALLOW MARINE CLASTICS SLOPE DEPOSITS AND CONFINED TURBIDITES SHALLOW TO OPEN MARINE Turonian transgression Senonian unc. Lower Miocene Oligocene unc. Upper Dakar Canyon TESTED RESERVOIR FIELD (or Reference Well) CHINGUETTI, THIOF, BANDA PELICAN DOME FLORE, DOME GEA DIAM NADIO GADIAGA DKM 2, RF 2 FAUCON ? - (CVM 1) JAMMAH 1 - (CVM 1, FAUCON) DKM 2 RF 3 - (CVM 1) SOURCE VG Ref. Well DSDP 367 CM 10 FAUC. ??? Oil Condensate Gas

HYDROCARBON OCCURRENCES & PRODUCTION Diam Niadio field Gadiaga field Dome Flore & Gea fields

217 393 033 Nm3 (7.6 Bcf) 62 642 bbs light oil 34° API HYDROCARBON OCCURRENCES & PRODUCTION Gadiaga field ~ 95 000 000 Nm3 ( 3.325 BCF ) producing since Oct 2002 ANNEE PRODUCTION DE GAZ (Nm3) CUMUL (Nm3) Octobre 2002 3 379 431 2003 12 637 561 16 016 992 2004 15 101 900 31 118 892 2005 15 936 769 47 055 661 2006 12 225 816 59 281 477 2007 10 865 236 70 146 713 2008 6 796 073 76 942 786 2009 17 114 983 94 057 769 Diamniadio field 217 393 033 Nm3 (7.6 Bcf) from 1987 to 2000 62 642 bbs light oil 34° API 35 692 bbls condensate 2009 : 17 114 983 Nm3 (~600 mmscft) 759 bbls condensate

DOME FLORE & GEA Heavy Oil in Oligocene limestones ( 10 – 13 ° API ~ 1Bbls ) Light Oil Maestrichtian ( 33° API ) Oil shows in Miocene & Albian sands Flore & Gea fields

GAS TRANSPORT NETWORK Gadiaga field Kabor storage and epuration station Gas Turbine at Cap des Biches 34 km - 10 km - 9 km Cement plant 11

CONTRACT AREAS Licenses 3 PSC offshore 3 PSC onshore 5 Companies 5 blocks under negotiation 5 open blocks offshore 3 open blocks onshore

REVIEW OF RECENT EXPLORATION ACTIVITIES

SEBIKHOTANE Avril 2003 DN-15B in 2006 commitment : 2 exploration wells Konkorong-1 Baobab-1

TAMNA 6 wells drilled the last two years Gas in Lower Senonian sands connected to transport system ~64 000 Nm3 to SOCOCIM cement plant presently ~ 300 000 Nm3 / day possible delivery to SENELEC power plant October 2006

Structural/Stratigraphic traps SAINT LOUIS offshore 60 % 30 % 10 % Structural/Stratigraphic traps west of the Cayar fault zone; Structural traps within the Cayar fault zone; Turbidites/mas flow deposits west the Cayar fault zone granted 2003 1200 km 2D Juillet 2004

Acquisition 620 km2 of 3D in March-April 2008 Ibis & Flamengo leads

SAINT LOUIS offshore profond 1500 Km 2D high frequency airmag survey 4225 Km2 5695 line Kms Satellite seep study economic evaluation (1.5 TCF)

CAYARS offshore blocks ~ 1690 km 2D on March 2006 Airmag survey March 2007

CAYARS offshore blocks December 2008

RUFISQUE offshore profond 2088 Km 2D Nov/Dec 2004 1500 km2 3D Jan/ Feb 2007 Relinquished by Edison/Petrobras

SANGOMAR - RUFISQUE 90 % 10 % 2050 km2 3D ( Feb - Mar 2007 ) November 2004

plays & leads N S N S L Cretaceous Carbonate shelf Margin play Top Aptian Senonian Unconformity Depth 3D line 1541 Albian Buried hills 3D Line 9076 Santonian fans N S Slope fan play Albian N S 3d Line 9076 Depth Prospective dip closed Interval Top Aptian High amplitude Upper slope Fan complexes Neocomian Senonian Unconformity 3d Line 1541 Depth Turonian

SENEGAL OFFSHORE SUD About 10 000 km of 2D from 1973 et 2001 8 wells

PALEOZOIC BASIN Prospective Area : East Meridian 16° Bassins intracratoniques Prospective Area : East Meridian 16° Surface : environ 60 000 km² Two sub-basins East Meridian 15°

PALEOZOIC BASIN

SENEGAL EAST AREA 2 bassins L1 et L2 identified Basin L1 L2 NiF-1 KrF-1 DiF-1 Basin L5 190 km H1 H2 H3 H4 H5 L1 L2 L6 L3 L4 Landsat 7 ETM+ ERS SAR

PETROLEUM LEGISLATION LEGAL AND FISCAL TERMS

LAW N° 98-05 of January 08, 1998 (PETROLEUM CODE) PRODUCTION SHARING CONTRACT (PSC) EXPLORATION Initial Period: 3-4 years Renewal Periods: 2-3 years EXPLOITATION PERIOD Initial Period: 25 years Extension Periods: 10+10 years

EXPLORATION WORK PROGRAM & EXPENDITURE OBLIGATIONS to be negotiated RETENTION PERIOD If a discovery is certified non commercial, Contractor may be granted a Retention Period of maximum: 3 years for crude oil 8 years for natural gas

PETROSEN’S PARTICIPATION Exploration phases: Carried Interest of 10 % After Commercial discovery: Working Interest up to 20 % FISCAL REGIME Twenty five per cent (25%) Income Tax ( applied on net profit )

Senegal Basin has generated oil and gas THANK YOU Senegal Basin has generated oil and gas Diamniadio, Gadiaga and Casamance Dôme Flore Presence of world class source rocks in Turonian-Cenomanian secondary good sources in Albo-Aptian and Jurassic Petroleum system in Deep water with various structural trends and traps 60 000 km2 underexplored Paleozoic basin with good reservoirs in Ordovician and Devonian and good source in Silurian, and traps and plays identified Law with flexible terms