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应用地质统计模型来产生并间三维岩相模型,然后在此三维岩相模型中进行流体流动模拟。重复研究地质调查资料与地质统计模型的主要特性,就可以对模拟试验和流体流动状况进行解释。
The geostatistical model was applied to generate inter-and inter-3D lithofacies models and the fluid flow simulations were then performed in this 3D lithofacies model. Repeated studies of the main features of geological survey data and geostatistical models allow interpretation of simulation tests and fluid flow conditions.