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Alwyn North Trassic Main gas-condensate: drilling deeper promotes production

机译:Alwyn North Trassic主凝析气:更深的钻探可促进产量

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Production of oil and gas in the Alwyn North Field, UKCS, commenced in 1987 from Middle Jurassic Brent and Lower Jurassic Stafjord reservoirs. In 1988, a deepened Stafjord producer well (3/9a-N21) detected gas in the underlying Triassic, but testing was not possible at that time. The 3/10b-2 exploration well, drilled in 1992 to the east of the field, tested gas at low rates from a poor quality Triassic reservoir section. In 1995 well 3/9a-N33, a deviated well, was drilled from the Alwyn platform to evaluate the productivity of the deep Triassic. This well penetrated 770 m of Upper Lunde section, which was tested at 1.3 X 10~6 m~3 per day of gas plus 4400 STB per day of condensate. The Alwyn trap comprises a westerly dipping fault panel structure. Erosion over the crest of the titled panel and the eastern-facing scarp slope by the Base Cretaceous Unconformity (BCU) truncates the Jurassic section down to the Upper Triassic. Sealing of the Triassic Main accumulation is by uppermost Triassic shales of the overlying Stafjord Formation and by Cretaceous mudrocks onlapping onto the BCU. Hydrocarbon charging of the Triassic Upper Lunde sandstones is from mature Late Jurassic Kimmeridge Clay source rocks that are juxtaposed against the reservoir along parts of the eastern frontal fault of the Alwyn panel. The Upper Lunde (of Carnian of Rhaetian age) is a low net: gross reservoir section up to 800 m thick. The sediments are of semi-arid fluvial, floodplain and lacustrine origins, with the best reservoirs occurring in fluvial channel sandstones. The Late Triassic comprises four informal zones from A (top seal), through B and C to D reservoirs, above the Middle Lunde shale. The Triassic reservoir fluids are gas-condensate in the B and C units with an intraformational seal at the C-D boundary, beneath which lies volatile oil in the D unit. A total of eight further Triassic production wells were added to the Alwyn North Field by the end of 2001, as the development plan for Triassic Main progressed. These wells contribute in the order of 60% to the Alwyn North daily production.
机译:1987年,UKCS的Alwyn North Field开始从中侏罗统布伦特和下侏罗统Stafjord油藏生产石油和天然气。 1988年,加深的Stafjord生产井(3 / 9a-N21)在底层的三叠纪发现了天然气,但当时无法进行测试。 3 / 10b-2勘探井于1992年在该油田以东钻探,以低速从劣质三叠系储层中测试了天然气。 1995年,在Alwyn平台上钻了3 / 9a-N33井,这是一口偏斜井,以评价深三叠纪的生产率。该井穿透了770 m的上隆德断面,以每天1.3立方米10〜6 m〜3的天然气和4400 STB的凝结水进行测试。 Alwyn陷阱包括一个西倾断层板结构。基部白垩纪不整合面(BCU)对标题板顶的侵蚀和朝东的陡坡,将侏罗纪的断层截断至上三叠统。三叠系主堆积的封闭是由上覆的斯塔夫峡湾组的最上三叠统页岩和重叠在BCU上的白垩纪泥岩组成的。三叠纪上隆德砂岩的碳氢化合物来自成熟的晚侏罗世金梅里奇粘土源岩,这些岩石沿阿尔文板块的东部前断层部分并排靠着储层。上隆德(Rheatian时代的Carnian时期)是一个低层网:储层总厚度达800 m。沉积物是半干旱河流,洪泛平原和湖相的起源,最好的储集层是在河流河道砂岩中。三叠纪晚期包括在隆德中页岩之上的四个非正式区域,从A(顶部海豹),B和C到D储层。三叠纪油藏流体在B和C单元中是凝析气,在C-D边界处具有内部构造密封,D单元中的挥发油位于其下方。到2001年底,随着Triassic Main的开发计划的进行,总共在Alwyn North油田增加了8口Triassic生产井。这些井为Alwyn North的日产量贡献了60%左右。

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