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Nested Stochastic Simulations:A New Approach in Assessing Spatial Distribution of Carbonate Sedimentary Facies and Associated Diagenetic Overprints

机译:嵌套随机模拟:一种评估碳酸盐沉积相空间分布及相关成岩套印的新方法

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A major challenge today is the development of carbonate reservoirs.They represent the most significant reservoir formation in the middle-east gulf region.In carbonate reservoirs,heterogeneity is usually driven by both depositional and diagenetic patterns.The complex diagenetic history which prevails in these reservoirs influences the final static and dynamicreservoir properties.Dolomitisation is one of the most crucial diagenetic phases because of the way in which it constrains the permeability behaviour of the field.Detailed diagenetic research has shown that various genetic dolomite types exist,including evaporative,mixed evolved sea-water-freshwater and late thermobaric.Defining static rock-type can therefore be problematic due to the highly imbricate diagenetic phases and their various distributions and extensions.A further major difficulty is the spatial distribution of rock-types in reservoir models,each linked to different sedimentological and diagenetic processes and each with their own,but interdependent,geometrical characteristics.In order to optimise the current production of reservoirs as well as future field development plans it is therefore necessary to understand the main diagenetic phases and develop approaches which effectively incorporate them into the static reservoir model.This paper presents a synthetic modelling workflow applied to a large oolitic ramp derived from outcrop and field observations.This new approach is based on nested stochastic simulations,geologically-driven and derived from the relationships between dolomite type,stratigraphic position,palaeogeographic position,depositional facies,and proximity to fault/fracture zones.In addition to the initial depositional model,three diagenetic phases are modelled successively in order to restore the complex spatial relationship existing between diagenetic alterations.The outcome of this modelling workflow,after a stage testing coherence with PC and Kr values and dynamic rock-typing definition,is fed into a dynamic simulator in order to assess the potential impact on field behaviour,production profiles and well productivity.
机译:今天的一项重大挑战是碳酸盐储层的发展。他们代表了中东海湾地区最重要的储层形成。碳酸盐储层,异质性通常由沉积和成岩图案引起的。在这些储层中占上去普遍的复杂成岩病史影响最终的静态和动态的性质。Dolomisation是最重要的成岩阶段之一,因为它限制了该田间的渗透性行为的方式。预先成岩性研究表明存在各种遗传白云岩类型,包括蒸发,混合的进化海因此 - 水 - 淡水和晚期热腐蚀。因此,由于高度覆盖的成岩阶段及其各种分布和延伸,静态岩型可以是有问题的。进一步的重大困难是储层模型中岩石类型的空间分布,每个难度是储层模型中的岩石类型不同的沉积物和成岩工艺和每个沉积物他们自己但相互依存的几何特征。为了优化当前的水库生产以及未来的现场开发计划,因此有必要了解主要的成岩阶段,并开发有效地将它们纳入静态储层模型的方法。本文呈现综合建模工作流程,应用于来自露出露天和现场观测的大型鲕粒斜坡。这项新方法是基于嵌套随机模拟,地质驱动和来自白云岩类型,地层位置,古地理位置,沉积相之间的关系。靠近故障/骨折区域。除了初始沉积模型之外,连续建模三个成岩阶段,以恢复成岩改变之间存在的复杂空间关系。该模型工作流程的结果,与PC和KR舞台测试相干值和动态摇滚键入defirio n,被馈送到动态模拟器中,以评估对现场行为,生产简档和生产率的潜在影响。

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