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A New Automated 3D Seismic Stratigraphic Methodology

机译:一种新型的自动3D地震地层学方法

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Seismic stratigraphic interpretation is a powerful method for analyzing the depositional history of the subsurface. However, the lack of support of such interpretation methods in the state-of-the-art tools limits its application. A novel technology allowing a highly automated procedure for seismic stratigraphic interpretation is presented. The technology includes an automated high resolution extraction step of all the stratigraphic primitives. The technology supports a “dual domain” concept that enables to interpret transparently in the seismic domain and the chronostratigraphic time domain. The interpreter controls this mapping by selecting the appropriate set of stratigraphic primitives to define this transformation. The high resolution extraction step is based on Borgos et al., 2003, 2005. The output from this classification results in extrema patches from which the stratigraphic primitives are defined. The method can be extended to active tectonic basins by including fault patches in the mapping (Pedersen et al., 2003, 2005). To demonstrate the potential of this new methodology we have applied it to an offshore Brazil case. The extracted stratigraphic surfaces are built from merged extrema patches. The obtained stratigraphic primitives refine the geological model and allow to accurately place the compartment boundaries and identify presence of hydrocarbons.
机译:地震地层解释是分析地下沉积历史的有力方法。但是,现有工具缺乏对此类解释方法的支持,限制了其应用。提出了一种允许高度自动化的地震地层解释程序的新颖技术。该技术包括所有地层基本要素的高分辨率自动提取步骤。该技术支持“双域”概念,该概念可以在地震域和年代地层时域中进行透明解释。解释器通过选择适当的地层基元集来定义此转换来控制此映射。高分辨率提取步骤基于Borgos等人(2003年和2005年)。此分类的输出结果是形成极值斑块,并从中定义了地层图元。通过在地图中包括断层斑块,该方法可以扩展到活动构造盆地(Pedersen等,2003,2005)。为了展示这种新方法的潜力,我们将其应用于巴西近海案例。提取的地层表面是根据合并的极值斑块构建的。所获得的地层原始数据完善了地质模型,并允许精确地划分车厢边界并识别出碳氢化合物的存在。

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