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Prospectus re Admission to the Official List - Heritage Oil

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RPS Energy<strong>Heritage</strong> <strong>Oil</strong> – Competent Persons Reportflow against <strong>the</strong> higher back-p<strong>re</strong>ssu<strong>re</strong>. The fo<strong>re</strong>cast for <strong>the</strong> West Bukha production start-up has beenassumed, conservatively, by RPS <strong>to</strong> be January 2009 although <strong>the</strong> Opera<strong>to</strong>r has advised <strong>Heritage</strong> thatproduction is targeted for 3 rd Quarter 2008. It has been assumed that Bukha will cease productiontemporarily while West Bukha p<strong>re</strong>ssu<strong>re</strong>s <strong>re</strong>main high.West Bukha will <strong>re</strong>ach a point when <strong>the</strong> flowing p<strong>re</strong>ssu<strong>re</strong> will be sufficiently low that <strong>the</strong> Bukha field wouldbe brought back in<strong>to</strong> production and both fields would produce at <strong>the</strong> same time through <strong>the</strong> samepipeline <strong>to</strong> <strong>the</strong> Ras Al Khaimah Gas Commission (‘‘RAKGAS’’) plant.3.3. West Bukha FieldThe West Bukha/Henjam gas field is located in <strong>the</strong> Straits of Hormuz approximately 22 km west of <strong>the</strong>Bukha field in about 90m of water. The field straddles <strong>the</strong> border between Iran and Oman. The field wasdiscove<strong>re</strong>d in 1975 by <strong>the</strong> Henjam-1 well in Iran and was subsequently appraised with Khasab-1, drilled byElf in Oman in 1977. Khasab-1 was drilled off structu<strong>re</strong> and encounte<strong>re</strong>d water. A second appraisal well,West Bukha 1, drilled in 1987 by IPC found gas condensate but at <strong>the</strong> time failed <strong>to</strong> produce commercialrates. The National Iranian <strong>Oil</strong> Company (NIOC) acqui<strong>re</strong>d 3D seismic over <strong>the</strong> field and approximately80 per cent. of <strong>the</strong> a<strong>re</strong>a cove<strong>re</strong>d was made available <strong>to</strong> <strong>the</strong> Block 8 licence holders.It is unders<strong>to</strong>od that attempts <strong>to</strong> negotiate a possible joint field development with Iran and Oman failed <strong>to</strong>produce an ag<strong>re</strong>ement. Although such negotiations a<strong>re</strong> continuing, <strong>the</strong> Block 8 partnership has sincedecided <strong>to</strong> pursue an Oman only development. <strong>Heritage</strong> advises that <strong>the</strong> Opera<strong>to</strong>r has secu<strong>re</strong>d ag<strong>re</strong>ementfrom <strong>the</strong> Sultan of Oman’s government <strong>to</strong> develop <strong>the</strong> field. However, public domain data from NIOC inIran suggests that an Iranian development is likely <strong>to</strong> proceed imminently. RPS is not in a position <strong>to</strong> opineon <strong>the</strong> legal status of <strong>the</strong> development.3.3.1. DatabaseThe West Bukha field is cove<strong>re</strong>d by 2D seismic acqui<strong>re</strong>d from 1974-1986, this data is poor quality. TheIranian National <strong>Oil</strong> Company acqui<strong>re</strong>d a 3D survey over <strong>the</strong> West Bukha field which covers <strong>the</strong> Omanand Iranian parts of <strong>the</strong> field. This survey is high f<strong>re</strong>quency in <strong>the</strong> upper section but very good quality at<strong>the</strong> <strong>re</strong>servoir depth. The West Bukha 3D has been depth migrated, this data was used prior <strong>to</strong> <strong>the</strong> drillingof <strong>the</strong> West Bukha-2 well whe<strong>re</strong> it was found that velocities had been inaccurately modelled. Well Datafrom four wells was made available, West Bukha-1, West Bukha-2, Henjam-1 and Khasab-1. Full log suiteswe<strong>re</strong> made available for <strong>the</strong>se wells as well as geological and test data. A static geological modelwas provided.3.3.2. Geology & GeophysicsThe field consists of a single contiguous NW-SE t<strong>re</strong>nding fault and dip closed structu<strong>re</strong> covering an a<strong>re</strong>a ofapproximately 62 sq km. Fractu<strong>re</strong>d carbonate <strong>re</strong>servoirs occur within <strong>the</strong> C<strong>re</strong>taceous Ilam, Mishrif,Mauddud and Thamama Formations at depths of between 3,600 and 4,200 m TVDSS. The<strong>re</strong> isconsiderable variation in thickness of <strong>the</strong> Ilam and Mishrif Formations linked <strong>to</strong> sedimentary depositionalong a carbonate shelf edge. The Ilam and Mishrif Formations a<strong>re</strong> thickest in Iran whe<strong>re</strong>, in Henjam 1,<strong>the</strong>y attained a gross thickness of mo<strong>re</strong> than 100 m whilst within <strong>the</strong> field boundary in Oman <strong>the</strong>seformations thin <strong>to</strong> around 50 m. The Mauddud Formation has an average thickness of approximately 80 mthroughout <strong>the</strong> field and is separated from <strong>the</strong> underlying Sabsab and Thamama Formations by <strong>the</strong> NahrUmr shale with an average thickness of 136 m. The Sabsab and Thamama <strong>re</strong>aches a <strong>to</strong>tal thickness ofaround 400 m.The Opera<strong>to</strong>r and <strong>Heritage</strong> have interp<strong>re</strong>ted th<strong>re</strong>e horizons across <strong>the</strong> West Bukha field; Top Ilam, TopNahr Umr and Top Thamama. The first two horizons define <strong>the</strong> structural envelope of <strong>the</strong>Mishrif-Mauddud <strong>re</strong>servoir (Figu<strong>re</strong> 9).(4) We note that this consequence has been p<strong>re</strong>viously igno<strong>re</strong>d. However, <strong>the</strong> opera<strong>to</strong>r has stated (Sept.07 OCM Minute) that heexpects Bukha production <strong>to</strong> cease once West Bukha comes on st<strong>re</strong>am.83

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