Advanced Meandering Fluvial Reservoir Characterisation for Static Model Improvement

H. Ismail, C. L. Lew, Muhd Rapi Mohamad Som, M. Kadir, M. Tajuddin
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Abstract

Modelling of meandering fluvial reservoirs with point bars and crevasse splays is very challenging. The conventional modelling approaches, especially for meandering fluvial reservoirs, are mainly controlled by wells, which have contributed to uncertainties in lateral variations between and away from well control. Integration of the improved sedimentology, geophysics and 3D reservoir geomodelling techniques of fluvial reservoir system are proposed in the study. In stratigraphic and structural framework building, the improved methodologies included 3D seismic geobody extraction, stratal slicing and high order architectural elements interpretation. 3D geobody extraction and stratal slicing technique enhanced interpreter ability to visualize fluvial features at specific time-equivalent stratigraphic surface. In lithofacies modelling, more refined high-order architectural elements were modelled using methodologies included 3D facies seismic probability, local varying azimuth and dip angle to capture lateral accretion of point bars inside the channels for better facies distributions following point bar architectures. In property modelling, porosity was populated using Gaussian Random Function Simulation constraint to lithofacies trend to control the distribution of porosity away from wells. This methodology resulted in the porosity distributions being well controlled following the lithofacies trend. The proposed workflows and methodologies enable geomodeller to produce a more geological realistic meandering fluvial reservoir model with internal lithofacies and property distribution honouring well data and input distribution.
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静态模型改进的高级曲流河储层表征
具有点坝和裂隙带的曲流储层的建模是非常具有挑战性的。传统的建模方法,特别是曲流油藏,主要由井控制,这导致了井控之间和远离井控的横向变化的不确定性。提出了河流储层系统的改进沉积学、地球物理和三维储层地质模拟技术相结合的方法。在地层和构造格架构建方面,改进的方法包括三维地震地质体提取、地层切片和高阶建筑元素解释。三维地质体提取和地层切片技术提高了解译人员在特定时间等效地层面上可视化河流特征的能力。在岩相建模中,使用包括三维相地震概率、局部变化方位角和倾角在内的方法对更精细的高阶建筑元素进行建模,以捕获河道内点坝的侧向增生,以便在点坝结构之后更好地分布相。在物性建模中,利用高斯随机函数模拟约束对岩相趋势进行孔隙度填充,以控制井外孔隙度的分布。该方法可以很好地控制孔隙度分布,使其遵循岩相走向。所提出的工作流程和方法使地质建模师能够生成一个地质上更真实的曲流河储层模型,该模型具有内部岩相和物性分布,符合井数据和输入分布。
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