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Integrated 3D Static Modeling of a Complex Carbonate Upper Shuaiba Reservoir, Block 9, Oman North

机译:集成3D静态建模,复杂的碳酸盐水库,第9块,阿曼北

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The field was discovered in 1992. It produces oil and associated gas from two reservoir sub units of the Upper Shuaiba USh3F1 and USh3F2, and exhibits both structural and startighraphical traps. The reservoir units are compartmentalized by NW-trending normal faults into five fault blocks within the same field towards the North East. They are vertically separated by non-reservoir low permeability mudstone facies. US3F2 is setting above Orbitolina shale. The objective is to build a new geological model in a very complex carbonate reservoir, to allow for better reservoir development, and adding new field opportunities using state of art seismic data. Lower unit (US3F2) consists of an aggradational sequence skeletal peloid-foram packstone/wackestone, and in-situ rudist-algal boundstone/packstone build-ups, which is localized to the NE-trending axis of the field. These sequences are deposited in a low to moderate energy environment. US3F2 reaches a maximum thickness of 50 ft in the rudist build-ups, but the width of the rudist-algal boundstone facies parallel to depositional dip (SE) is only 0.5-0.7 km. Cores exhibit abundant secondary porosity with an average of 30% and permeability up to 700 mD suggesting early subaerial exposure and leaching. Upper unit (US3F1) is either absent or very thin across the crest and thickens to over 20 ft basinward; downdip, it is separated from US3F2 by a shale unit. US3F1 consists of an upward-shallowing deposits of Orbitolina mudstone, reworked stromatoporoid-rudist floatstone, small rudist floatstone, and fine skeletal grain-dominated packstone with rudist fragments. 3D model was generated covering large area of about 15x9km of the field. The new seismic horizon and faults interpretation were used in the 3D structural modeling. Cores descriptions and photos were used to define core facies, depositional environments and vuggy intervals. Rudist buildups direction of progradation was also defined based on BHI. Reservoir rock Fabric number (RFN) was defined based on Lucia method and populated using veriogram per zone for the vertical wells using moving average method followed by Gaussian Random simulation, co-kriged with the moving average properties as a trend, for both vertical and horizontal wells. Porosity was populated with the same method. Water saturation and permeability were calculated using Lucia height function method. Understanding of the reservoir heterogeneity, architecture and 3D modeling using RFN based on Lucia method allowed a better distribution of reservoir properties to be used in dynamic simulation for better history match, predict waterflood performance and adding new development areas.
机译:该领域于1992年发现。它产生来自上舒瓦USH3F1和USH3F2的两个储层子单元的油和相关气体,并展示结构和活泼的陷阱。通过NW-Trowing常规故障将储存器单元分区,进入与东北部的相同领域内的五个故障块。它们被非储存器低渗透率泥岩相垂直分开。 US3F2是在Orbotolina Shale上面设置的。目标是在一个非常复杂的碳酸盐储层中建立一个新的地质模型,以允许更好的水库发展,并使用艺术地震数据的状态增加新的现场机会。下单位(US3F2)由一条骨干序列骨架Peloid-Foram Packstone / Wackestone以及原位粗鲁斯 - 藻石边界/包装石积累,其本地化为该领域的Ne趋势轴。这些序列沉积在低至中等能量环境中。 US3F2在粗鲁的建筑物上达到50英尺的最大厚度,但粗鲁斯 - 藻错石面相平行于沉积浸(SE)的宽度仅为0.5-0.7公里。核心具有丰富的二级孔隙率,平均为30%,渗透率高达700 MD,表明早期的底栖曝光和浸出。上部单元(US3F1)无论是不存在的还是非常薄的波峰,均匀地变稠于20英尺的盆地;下降,它由页岩单元与US3F2分开。 US3F1由胰酸碱泥岩的储存,重新加工的Stromatoporoid-rudist Floatstone,小粗鲁斯漂浮石和细骨骼晶粒主导的包装,与粗鲁斯碎片的储层。 3D模型被产生覆盖大约15x9公里的领域。新的地震地平线和故障解释用于3D结构建模。核心描述和照片用于定义核心相,沉积环境和vuggy间隔。 Rudist Baseups促进方向也基于BHI定义。基于Lucia方法定义了储层岩石面料数(RFN),并使用移动平均方法使用移动平均水平的垂直井的每个区域使用VirioMugum来填充,以及垂直和水平的移动平均属性共克里奇。井。用相同的方法填充孔隙率。利用Lucia高度函数方法计算水饱和和渗透性。了解基于Lucia方法的RFN的储层异质性,架构和3D建模的理解允许更好地分布在动态模拟中用于更好的历史匹配的动态模拟,预测水运性能并添加新的开发领域。

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