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现代沉积环境提供了明确的地貌数据,可用于对地下地层的各种特征进行量化的地质解释。传统的三维地质解释局限于一维和二维的基础数据:通常是钻井和露头数据。然而,河流三角洲系统地貌分析的成果通常只是反映不连续的沉积单元的分布规模。这些参数在调整储层模型中沉积单元的面
Modern depositional environments provide well-defined geomorphological data that can be used to quantify geological interpretations of various features of underground formations. Traditional three-dimensional geological interpretation is limited to one-dimensional and two-dimensional basic data: usually drilling and outcrop data. However, the results of the landscape analysis of the river delta system usually only reflect the distribution of discrete sedimentary units. These parameters are used to adjust the face of the depositional unit in the reservoir model