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ASSESSMENT OF FACIES DISTRIBUTION IN CARBONATE FIELDS USING STRATIGRAPHIC FORWARD, DIAGENETIC AND SEISMIC MODELLING

机译:利用地层向前,成岩和地震造型评估碳酸盐田区的相分布

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Carbonate rocks are usually very good carbonate reservoirs and can host giant fields, such as the Ghawar, Karachaganak or Lula fields. They can form in various depositional environments, stratigraphic and structural settings, and can be affected by many different diagenetic processes. As a result, they present very heterogeneous petroacoustic characteristics and are difficult to image and interpret even using up-to-date seismic data. Exploration and development of such reservoirs require to develop novel integrative approaches to better understand the regional-to-local sedimentological and diagenetic processes, which have shaped these reservoirs. The challenge of our study was to develop and run a fast and accurate workflow combining seismic interpretation, detailed sedimentological and diagenetic studies of wireline logs and core data, with deterministic stratigraphic forward and synthetic seismic modelling of a carbonate reservoir (average thickness of about 200 m) at an appraisal scale (650 km~2, using a grid point spacing of about 200 to 500 m). A review of borehole and seismic data, and in particular lithofacies classification (facies type and facies group) and EOD definition (Environments Of Deposition), allowed us to define stratigraphic parameters such as accommodation space, carbonate production rates, sediment transport parameters, dissolution-cementation rates, ... A series of numerical simulations were performed using the DionisosFlow stratigraphic model to simulate sedimentological and diagenetic processes through geological time. The simulation results were compared to the wireline and seismic data using the "stratigraphic model to seismic data" prototype until reaching a reasonable match between simulated and interpreted sediment proportions inside each flow unit. Finally, sensitivity analysis was performed. This stratigraphic forward and seismic modelling approaches made it possible to better understand the impact of sedimentary and diagenetic processes on large-scale carbonate reservoir properties and finally to reduce uncertainties on the appraisal-scale reservoir characterization.
机译:碳酸盐岩通常是非常好的碳酸盐岩储层,并且可以承载巨大的领域,如加瓦尔,卡拉恰甘纳克或卢拉领域。它们可以形成各种各样的沉积环境,地层和结构设置,并且可以通过许多不同的成岩过程的影响。其结果是,它们呈现非常不均匀petroacoustic特性和难以成像,甚至使用上最新的地震数据解释。勘探及水库等的发展需要开发新的综合性的办法,以更好地了解地方对本地沉积学和成岩过程,它塑造了这些水库。我们研究的挑战是开发和运行一个快速,准确的工作流程地震解释,详细的电缆测井和核心数据的沉积学和成岩研究,结合确定性地层向前和碳酸盐岩储层的合成地震建模(约200 m 2的平均厚度)在评价尺度(650公里〜2,使用约200至500微米的网格点间距)。井眼和地震数据,特别是岩相分类(相型和相组)和EOD定义(环境沉积)的综述,使我们能够确定地层参数,如容置空间,碳酸生产速率,沉积物传输参数,溶解 - 胶结率,...利用DionisosFlow地层模型来模拟地质时期沉积学和成岩过程中进行了一系列数值模拟。仿真结果进行了比较,使用“地层模型以地震数据”的原型,直到到达每个流动单元内的模拟和解释沉渣的比例之间的合理匹配的有线和地震数据。最后,进行灵敏度分析。这种地层前和地震建模方法使我们能够更好地理解和沉积成岩过程对大型碳酸盐岩储层性质的影响,并最终降低了评价尺度油藏描述的不确定性。

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