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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 Report3.2. Bukha FieldThe Bukha gas field is located in <strong>the</strong> Straits of Hormuz approximately 12 km off <strong>the</strong> west coast of <strong>the</strong>Musandam Peninsula. The field was discove<strong>re</strong>d by IPC in 1979. Th<strong>re</strong>e wells have been drilled on <strong>the</strong>structu<strong>re</strong>. Bukha-1 and Bukha-2 a<strong>re</strong> situated close <strong>to</strong> <strong>the</strong> c<strong>re</strong>st of <strong>the</strong> structu<strong>re</strong>. Bukha-3 was drilleddi<strong>re</strong>ctionally from <strong>the</strong> Bukha-1 surface location down flank <strong>to</strong> <strong>the</strong> southwest. The field has been onproduction from two wells, Bukha-1 and -2, since 1994.3.2.1. DatabaseThe Bukha Field is cove<strong>re</strong>d by 2D seismic data that was acqui<strong>re</strong>d over a considerable span of time from1974 <strong>to</strong> 1986. These data have been <strong>the</strong> subject of a <strong>re</strong>processing exercise in 2001. Despite this<strong>re</strong>processing numerous problems still exist of <strong>the</strong> type <strong>to</strong> be expected with 2D data in a<strong>re</strong>as of high dipsnamely migration misties, out of plane <strong>re</strong>flections etc. A 3D survey was acqui<strong>re</strong>d during 2006/07, but is stillbeing processed by <strong>the</strong> opera<strong>to</strong>r.Production data from <strong>the</strong> field we<strong>re</strong> provided by <strong>Heritage</strong>.3.2.2. Geology and GeophysicsThe field consists of a single contiguous NE-SW t<strong>re</strong>nding fault and dip closed structu<strong>re</strong> covering an a<strong>re</strong>a ofapproximately 35 sq km. The tilted fault block is controlled by two main faults; <strong>the</strong> Tibat thrust and <strong>the</strong>Bukha back-thrust. Fractu<strong>re</strong>d carbonate <strong>re</strong>servoirs within <strong>the</strong> C<strong>re</strong>taceous Mauddud and ThamamaFormations occur at depths of between 2,900 and 3,500 m TVDSS. The Mauddud Formation has anaverage thickness of 52 m and is separated from <strong>the</strong> underlying Thamama Formation by <strong>the</strong> Nahr Umrshale with an average thickness of 106 m. The Thamama <strong>re</strong>aches a <strong>to</strong>tal thickness of around 650 m.Figu<strong>re</strong> 5 shows a depth structu<strong>re</strong> map of <strong>the</strong> Bukha Field. The a<strong>re</strong>a above structural spill that lies <strong>to</strong> <strong>the</strong>north of <strong>the</strong> North Bukha fault is known as North Bukha and it is not known whe<strong>the</strong>r this a<strong>re</strong>a is beingdrained by <strong>the</strong> production wells. If it becomes appa<strong>re</strong>nt that <strong>the</strong> <strong>re</strong>serves in <strong>the</strong> North Bukha a<strong>re</strong>a a<strong>re</strong> notbeing produced <strong>the</strong>n an appraisal well may be drilled.Figu<strong>re</strong> 5:Bukha Field—Top Reservoir Depth Map21FEB20082315000779

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