Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
PETROLEUM POTENTIAL OF THE ALBERTINE GRABEN, UGANDA, CONFIRMED Presented By Reuben Kashambuzi Commissioner, Petroleum Exploration and Production Department, Uganda at the AAPG Convention 2006, Houston, Texas, USA PRESENTATION OUTLINE 1. Regional Setting of the Albertine Graben • EARS • Volcanism 2. Structural Setting 3. Hydrocarbon Play Indicators • • • • Source rocks Reservoirs Traps Seals 4. Concluding Remarks • Key facts about Uganda • Investment Opportunities REGIONAL SETTING The EARS bifurcates into two arms Ethiopian rift Eastern and Western arms separated by Tanzanian Craton Albertine Graben Northern most part of the Western arm of the East African Rift System 500 Km long, averaging 45 km wide and 23,000 sq km Volcanic processes are not widespread in the Western arm as they are in the Eastern arm Tanzanian Craton EARS STRUCTURAL SETTING 25000 0 25000 30°30' 50000 31° 31°30' 32° 32°30' Sudan 75000 metres oma in 3°30' Arc 1960 / UTM zone 36N LEGEND Rift sedim ents -160 -150 3° 3° No r ther nd 5 -160 -160 2°30' -180 Gravity depocentre 2°30' Mesozoic Basin 1 R. Nile Norm al fault -200 Continental Extension – NW-SE Strike slip 30° -180 29°30' 3°30' Grabens and half grabens separated by accomodation zones Graben strongly shaped by; 0 -17 Accom odation zone ny i Wa ki ic Ka se R. Kafu nd a m oc r of atic Co R ng epu o bl De La ke A lb e rt 2° 1°30' 0°30' oma i Lake Victoria 8 - -1 1 7 7 0 0 5 Northern & Southern Domains: Oblique Extension 1 0°30' Sou Lake George th e rn d an ug ur u vo lc 4 6 5 ny ar Lake Edward - 01 os K a twe K ik o ro n g o -1 6 0° Central Domain: Orthogonal extension Bu 0° n R. Se m li k i 0°30' 0°30' U ga 1° 0 1 0 - 2 3 n Ce 1° Northern trends in a NNE-SSW Central trends in a NE-SW Southern trends in a NNE-SSW ain m o ld tra 0 - 2 2 1°30' Three structural domains: - 22 0 0 1 0 a sw M Oil Seep Volcanics 2° Relay ram p 29°30' 30° 30°30' 31° 31°30' 32° 32°30' Summary tectonic map of the Albertine Graben HYDROCARBON PLAY INDICATORS Source Rocks: Rocks with good source potential have been mapped in the Graben e.g. Kaiso Tonya. Good source rocks reported in the Waki-B1, Turaco, Mputa and Waraga wells Inferred from oil seeps High quality lacustrine mature source rocks encountered in the wells drilled on the Turaco, Mputa and Waraga prospects. Kaiso-Tonya shale HYDROCARBON PLAY INDICATORS Cont’d ☼ ☼ Turaco-2 Lithology log. Good source rocks were reported in the well Waki B-1 Lithology log. Excellent source rocks were encountered HYDROCARBON PLAY INDICATORS Cont’d Oil Seepages Paraa Distributed along the entire length of the Albertine Graben Different geochemical characteristics indicating multiple sourcing Sonso Runga Kibiro LAKE ALBERT Kaiso Tonya Confirmed Oil Seeps Reported Oil Seeps Kibuku Oil Seeps interpreted from Radar Imagery 0 10 20 30Km Radar Imagery of the Albertine Graben showing interpreted and confirmed oil seeps HYDROCARBON PLAY INDICATORS Cont’d GEOLOGY MAP OF KAISO-TONYA AND BUTIABA AREA 260000 30000 290000 280000 270000 310000 320000 330000 340000 350000 Oil Seepages 360000 Pakuba ± Porombo Panyimur O VIC T ^_ I LE A N< RI & ^_^_ Paara < & R. Z ^_ o i la ^ ^_ _ Wanseko Oil Seepage in highly crushed basement at the Kabyosi oil seep in Kaiso – Tonya area R. S Bulisa am b iy R. Z oliya o l iy a Katara e R. Z Wairingo Camp ig a Oil film floating on the Victoria Nile a R. W Kabira Bugoigo R. ai R. W soke To Masindi S onso ^` & < Butiaba 200000 T ER Waki R. W B AL KE LA aki^` Biso Runga Runga 1 190000 Runga 2 Kibiro HOIM Legend _ & < R. K it awe O To Hoima H oi R. mo Tonya Point 190000 Kibiro 2^ <^_ & ^_ & < <^_ & 180000 Oil seep from shallow well at Kibiro To Masindi <^_ ^_& & < 310000 R.W Kaiso YA HUN TING AREA by a amba KAISO TON BISERUKA 170000 Surficial Deposits Quartizites Road Kaiso Formation Gneiss Path Sebugoro Formation Schists Rivers Upper Warwire Formation Diorites Fault Warwire Formation Gabbros < & Oil Seep Nkondo Formation Calcic Silicates ^_ Station Point Laterite Eclogites % Waki well 170000 To HOIMA R.H 300000 oh wa NYAMASOGA Sebugoro ^_ ^_KABAALE 160000 Nkondo^_ R. ^^_ _ W ar ^_ 260000 ^_ ^_ & < ^_ ^_ 160000 290000 Mafic Intrusives To KIZIRA-NFUMBI wire ^& <^_ ^_ & <_ & <^_ & < 0 KASEETA 270000 TO KABWOYA 280000 10 20 40 60 80 23 Oil impregnated channel Hoima Basin sandstone of the Kaiso FM on 100 the banks of R. Hohwa Kilometers HYDROCARBON PLAY INDICATORS Cont’d Reservoir rocks: Thick (100-200m) and well sorted sandstones Good porosities of the order of 30% Good permeability Multiple pay zones confirmed by drilling (Mputa-1 and Waraga-1) Sebugoro Formation Hohwa oil sandstone Kisegi Formation HYDROCARBON PLAY INDICATORS Cont’d Traps: Residual gravity anomaly map of EA2, showing distribution of gravity highs oil seepages and well locations Sedimentary structures in the Graben are basement related Residual gravity anomalies reveal several structures Structures have been confirmed by seismic data and tested by exploration drilling Compares well with Sudan where major oil fields coincide with gravity highs HYDROCARBON PLAY INDICATORS Cont’d Semliki structures Saddlebill Residual gravity anomaly map of Semliki Basin, EA3A Turaco-1,2&3 drilled on a gravity high Turaco – Encountered natural gas contaminated with CO2 in the ratio CH4 : CO2 of 1:4 Good reservoirs High flow rates (60 mmcft/d) Good seals Good source rock quality Multiple reservoirs Shallow biogenic (?) gas (600700m depth) CO2 not extensive Gravity reveals other significant subsurface structures also confirmed by seismic HYDROCARBON PLAY INDICATORS Cont’d Kaiso-Tonya structures Mputa and Waraga Prospects tested by exploration drilling GEOLOGY OF KAISO - TONYA AREA 270000 280000 S ab mb ya a Shows in fractured basement Wells cased and suspended for re-entry for testing re oro Thin sandstones ar wi S abyosi Nkondo W Surficial Deposits Quartzite Kaiso Formation Gneiss Sebugoro Formation Hoima Basin Upper Warwire Formation Fault Warwire Formation Motorable Path Minor River Nkondo Formation R .K Multiple reservoirs Legend r w Hoh S R. Mputa #1 Sebugoro 160000 Wa S g bu Se R. Oil samples extracted for lab. analyses . R Kaiso 170000 R iv e ± Tonya Point Rich shales Oil shows 310000 S 180000 Waraga #1 Kibiro 300000 290000 1 Major River Laterite S Mafic intrusives + U Villages Seepage 14B + U + +U U 0 5 10 KM General geology of Kaiso-Tonya showing the Mputa and Waraga well location Copyright: Petroleum Exploration and Production Department, Marc HYDROCARBON PLAY INDICATORS Cont’d Kaiso-Tonya structures Mputa and Waraga Prospects coincide with significant gravity highs The gravity structures have been confirmed by seismic data Prospectivity of other structures still to be confirmed Residual gravity anomaly map of Kaiso-Tonya, EA2 HYDROCARBON PLAY INDICATORS Cont’d Amplitude 30000.000 20000.000 10000.000 0.000 -10000.000 -20000.000 -30000.000 Typical traps Flower Structures ts-HOG 2001 02 CMP Shot 0.00 19 110 39 120 59 130 79 140 99 150 119 160 139 170 159 180 179 190 199 200 219 210 239 220 259 230 279 240 ts-HOG 98 01 299 250 319 260 339 270 359 280 379 290 399 300 419 310 439 320 459 330 479 340 499 350 519 360 539 370 559 380 579 390 ts-HOG 2001 01 599 400 619 410 639 420 659 430 679 440 699 450 719 460 739 470 759 480 779 490 799 500 819 510 839 520 859 530 879 540 899 550 919 560 939 570 959 580 979 590 999 1019 1039 1059 1079 1099 1119 600 610 620 630 640 650 660 0.50 Rollover anticlines 1.00 Inversion anticlines 1.50 Potential for stratigraphic traps 2.00 2.50 Seismic section showing an inversion anticline in Semliki Basin HYDROCARBON PLAY INDICATORS Cont’d Amplitude 0.000 -3999999999999999900000000.000 -7999999999999999900000000.000 -11999999999999998000000000.000 -15999999999999998000000000.000 -19999999999999998000000000.000 Traps Cont’: CMP Shot 0.00 7326 4640 A -HLA 03 021 7166 4560 7006 4480 B A -HLA 03 023 6846 4400 A -HLA 03 025 6686 4320 6526 4240 A -HLA 03 027 6366 4160 A A -HLA A03 -HLA 029 05-09_filtmig A -HLA 03A081 -HLA A -HLA 03 A -HLA 031 05-1 A -HLA 03 5_filtmig A 083 -HLA 05-17X_filtmig 03A085 -HLA 03 033 6206 4080 6046 4000 5886 3920 5726 3840 5566 3760 5406 3680 A -HLA 03 035 5246 3600 A -HLA 03 037 5086 3520 4926 3440 A -HLA 03 039 4766 3360 0.50 1.00 1.50 2.00 2.50 3.00 Syncline 3.50 Inversion Anticline 4.00 5 Km Structural highs observed on the seismic sections are potential hydrocarbon traps - inversion anticlines Structural lows represent possible ‘Kitchens’ 4606 3280 A -HLA 03 041 4446 3200 4286 3120 A -HLA 0 4126 3040 HYDROCARBON PLAY INDICATORS Cont’d Seals: M BUTIABA WAKI FT WELL TD 4058' BASEMENT OIL AND POSSIBLE GAS __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 0 0 0 0 0 O 200 O O 0 0 300 0 O 1000 0 O 0 O O O O 0 O 0 O O 0 O 0 O __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 400 0 0 0 O 0 0 0 0 O 0 O 0 O O 0 0 SEEPS ARE KNOWN ON O 0 0 0 O 0 O 0 0 0 O 0 0 O O 0 O 0 0 O 0 0 O 0 0 0 O 0 O 0 O 0 500 0 0 O 0 KAISO FORMATION 100 1500 LACUSTRINE SANDS AND CONGLOMERATES __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 1720' __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ KISEGI FORMATION 2000 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 700 2500 __ __ __ __ __ __ __ __ __ __ 800 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 900 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 3000 1000 O O 0 0 O 0 O 0 0 0 O 0 O 0 O 0 0 O 0 Observations from Turaco, Mputa and Waraga exploration wells confirm effective seals 1100 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ WAKI JURASSIC __ __ __ __ __ __ __ __ __ __ 3500 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 1200 __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ 4000 0 0 0 OO 0 O 0 O O 0 THE OIL SEEPS MAY BE OF TWO KINDS. -THE SUDANESE HIGH WAX, HIGH POUR POINT. SOURCED FROM LACUSTRINE SHALES. - A MORE PARAFFINIC SEEP? SOURCED FROM MORE MARINE SHALES. FLUVIO LACUSTRINE WITH SOME BITUMINOUS SHALES BITUMINOUS SHALE 0 O O THE SURFACE. SANDS AND SHALES O 0 FORMATION 600 LOWER MIOCENE TO PLIOCENE Wide spread clays, some quite thick, provide regional seals. Clays have been mapped across the Albertine Graben __ __ __ __ __ __ __ __ __ __ 500 TERTIARY PLAYS, PRODUCTION AND SHOWS __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ EARLY PLEISTOCENE Alternating shales and sandstones observed in Waki-B1 well suggest good sealing mechanism QUATERNARY 3320' BITUMINOUS SHALE FLUVIO LACUSTRINE CLASTICS POSSIBLY EQUIVALENT TO UPPER IN THE WELL AT 3850' A SAND WITH ASPHALTIC OIL WAS FOUND, NO TEST. JURASSIC STANLEYVILLE FORMATION OF THE CUVETTE CONGOLAISE. 4008' BASEMENT Waki B-1 well lithology. Oil shows were encountered at 3850 ft KEY FACTS ABOUT UGANDA Population Size: 27 million people Size of country: 241,038 Sq. Km GDP: US$ 6.8 Billion Export Earnings: US$ 547.5 Million (2004) Fuel Consumption: 681,248.8 m3 (US$ 156.9 m/year), 2005 Installed Capacity: 300 MW of electricity Available Power: 140 - 220 MW of electricity Power demand: ~ 500 MW of electricity Power shortage: Effect of prolonged drought Thermal Generation: 50 MW to increase to 200 MW (End 2006) Confirmation of shallow gas in Turaco would alleviate the problem INVESTMENT OPPORTUNITIES PETROLEUM EXPLORATION AREAS 1, 2, 3A, 3B, 4 & 5 30 E 4 N4 N 4N MOYO Rail % Boundary of Exploration Area National Boundary Exploration Area 3 NIMULE Waki Well ! Oil Seepage I. Hotel p AirStrip Rhino Camp Basin p B E RT NI LE I. AL ± a) b) IC TO RI A NI LE ! < < BUTIABA < < p % I. < < K Hohwa ! !! << < LA 2 I. HOIMA R.KAF U I. I. p FORT PORTAL MUBENDE R.KATONGA KASESE • EA3B Semliki Basin • Size: 1,795 Sq. Km 0 • Not licensed L.GEORGE 0 Lakes Edward & George Basin I. • EA2 Lake Albert Basin • Size: 4,675 Sq. Km • Licensed: Hardman Resources (U) Ltd on 8st October 2001 • EA3A 1Semliki Basin N • Size: 1,982 Sq. Km • Licensed: Hearitage Oil and Gas and Energy Africa on 8th Sept 2004 3B < ! IK I KIBUKU UGANDA Semliki Basin Turaco Prospect Area MASINDI < Runga ! KIBIRO ! ! E ! 2N Sonso WAKI-1 RT A BE ! 3A Gas condensate Shallow biogenic gas High quality reservoir conditions established KASENYI < DEMOCRATIC REPUBLIC OF CONGO L < ! ML ! ! MSWA 1N V I. Northern Lake Albert Basin SE p ! PAARA R. 1 1 GULU • EA1 Packwach Basin • Size: 4,285 Sq. Km • Licensed: Heritage Oil and Gas (U) Ltd on 1st July 2004 Pakwach Basin < NEBBI Exploration Area 3B 1,795 Sq. Km 390 Sq. Km of 3D seismic data 410 Line Km of 2D seismic data Lithology and wire line data from 3 wells Structures with potential for ; p I. 2N • EA5 Rhino Camp Basin • Size: 6,040 Sq. Km • Licensed: Neptune 3N Petroleum (U) Ltd on 27th Sept 2005 5 ARUA 3N A Road Exploration Area 4 SW Rift Sediments R.A 5,910 Sq. Km Acreage on land and on the lake Geological & Geophysical data Sediment thickness, over 4 Km SUDAN Legend Exploration Area 4 32 E 31 E < AVAILABLE ACREAGE p LAKE I. EDWARD MASAKA 4 LAKE I. p MBARARA • EA4 Lakes Edward-George Basin • Size: 5,910 Sq. Km • Not yet1 S licensed VICTORIA 1S 30 E 31 E 0 32 E 25 50 75 100 125 Km PLEASE CONTACT Uganda Booth No. 461 at the International Pavilion OR. The Commissioner, Petroleum Exploration and Production Department, 21–29 Johnston Road P. O. Box 9, Entebbe (Uganda) Tel:+256 041 320714 Email: [email protected] Website: www.energyandminerals.go.ug THANK YOU