Prospectus re Admission to the Official List - Heritage Oil
Prospectus re Admission to the Official List - Heritage Oil
Prospectus re Admission to the Official List - Heritage Oil
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RPS Energy<strong>Heritage</strong> <strong>Oil</strong> – Competent Persons ReportThe installation and commissioning of new facilities of appropriate size for <strong>the</strong> production, processingand transportation of <strong>the</strong> produced oil; (<strong>Heritage</strong> advise that CND’s plan is cur<strong>re</strong>ntly in front of<strong>re</strong>gula<strong>to</strong>rs for <strong>the</strong>ir approval)The raising of sufficient capital funds <strong>to</strong> cover <strong>the</strong>se development costs.4.5. Facilities and CostsCommercial production commenced in 2007 on a small scale from two wells. The cur<strong>re</strong>nt plan is <strong>to</strong> drill up<strong>to</strong> 84 producers in <strong>the</strong> p50 case along with 46 Water Injection wells for <strong>re</strong>servoir support. Two drilling rigswill eventually be <strong>re</strong>qui<strong>re</strong>d with a planned 16 wells in years 2010 <strong>to</strong> 2012. The p50 Case is expected <strong>to</strong>produce over 60 MMstb peaking at about 16,000 bopd in 2014. Capital expenditu<strong>re</strong> (facilities costs) for <strong>the</strong>most likely case is estimated at US$180 MM including a 20 per cent. contingency. The 130 wells will bedrilled at a cost of average US$2 MM each. In <strong>the</strong> p10 case, with over 200 wells. RPS has assumed anadditional drilling rig is <strong>re</strong>qui<strong>re</strong>d from 2011. Production would be over 170 MMstb with a capitalexpenditu<strong>re</strong> of over US$300 MM. Operating costs a<strong>re</strong> assumed <strong>to</strong> be US$12 MM per annum during <strong>the</strong>plateau years plus a fur<strong>the</strong>r US$1.5 MM per annum for G&A.5. UGANDA—BLOCKS 1 & 3A5.1. OverviewUgandan Block 3A is located in <strong>the</strong> south of Lake Albert and covers <strong>the</strong> sou<strong>the</strong>rn part of <strong>the</strong> Ugandan sideof Lake Albert. Block 1 is located on land <strong>to</strong> <strong>the</strong> north of Lake Albert. Lake Albert is a largest lake in <strong>the</strong>nor<strong>the</strong>rn sec<strong>to</strong>r of <strong>the</strong> Western Rift. The lake surface is approximately 618 m above sea level and its riftedmargins a<strong>re</strong> mo<strong>re</strong> than 2,200 m above sea level in <strong>the</strong> west and mo<strong>re</strong> than 1,300 m in <strong>the</strong> east. He<strong>re</strong>, <strong>the</strong>graben has an average width of 45 km and is approximately 190 km long. Whilst many of <strong>the</strong> Western Riftsegments contain deepwater lakes, such as Lake Malawi (750 m) and Lake Tanganyika (1,500 m), LakeAlbert has <strong>re</strong>latively shallow water depths (approximate maximum of 60 m) but is believed <strong>to</strong> have similarsediment thicknesses as <strong>the</strong> o<strong>the</strong>r lakes.The Albert Basin is <strong>the</strong> most petroleum prospective a<strong>re</strong>a in Uganda and is a classical active rift basin of <strong>the</strong>East African Rift system.5.2. Data AvailableThe seismic database in Block 3A comprises 16 widely spaced 2D seismic lines of varying vintages2003-2005. The data quality in <strong>the</strong> nor<strong>the</strong>rn half of <strong>the</strong> block is fair with well defined <strong>re</strong>flections down <strong>to</strong><strong>the</strong> base of <strong>the</strong> Tertiary basin fill. To <strong>the</strong> south of <strong>the</strong> block <strong>the</strong> <strong>re</strong>gional data becomes inc<strong>re</strong>asingly poor andmapping of <strong>the</strong> deeper levels is particularly difficult. A 3D survey also exists over <strong>the</strong> Kingfisher discoverycovering 450 sq km along <strong>the</strong> south eastern lake sho<strong>re</strong>, data quality is <strong>re</strong>asonable. Shallow data atKingfisher lose cohe<strong>re</strong>ncy but this is above <strong>the</strong> zones of inte<strong>re</strong>st in <strong>the</strong> wells. Well data from 3 wells;Kingfisher-1, Kingfisher-1A and Kingfisher-1B we<strong>re</strong> made available. Full log suites we<strong>re</strong> made availablefor <strong>the</strong>se wells as well as geological and test data.Block 1 is cur<strong>re</strong>ntly cove<strong>re</strong>d by 17 2D seismic lines across <strong>the</strong> sou<strong>the</strong>rn portion of <strong>the</strong> block. Data quality isgenerally very good with <strong>re</strong>tention of amplitudes, cohe<strong>re</strong>nt <strong>re</strong>flec<strong>to</strong>r packages and fairly crisp faultterminations. As noted above, seismic acquisition in Blocks 1 and 3A is not due for completion untilMarch 2008. Much of <strong>the</strong> a<strong>re</strong>a outside <strong>the</strong> 3D seismic in Block 3A will be cove<strong>re</strong>d by additional infill 2Dlines and data will be available for <strong>the</strong> nor<strong>the</strong>rn part of Block 1A.Tullow has been exploring a fault terrace in Block 2, <strong>to</strong> <strong>the</strong> north of <strong>Heritage</strong>’s Block 3A and has a numberof <strong>re</strong>ported discoveries but RPS has no access <strong>to</strong> data from <strong>the</strong>se wells.105