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GeoTime~(TM): A Novel, Automatic 3D Chronostratigraphic Seismic Interpretation Methodology for Complex Geological Settings

机译:地理工史〜(TM):复杂地质环境的新型,自动3D计时器地震震动震动方法

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Chronostratigraphic seismic interpretation provides insights into basinal evolution. By mapping the internal stratigraphic architecture, this method has been widely used for well placement optimization and reservoir model building. Over many years of research at TOTAL, the Sismage team has created GeoTime?, a software tool for automatic chronostratigraphic analysis of seismic data, particularly in complex geological settings. This tool can be used to automatically or semi-automatically track the chronostratigraphic surfaces. The output is a 3D cube of stratigraphic surfaces (iso-geological time) which can be used to build the frame work for geomodels. A 3D cube of “Wheeler Diagram” is also obtained by segmenting the seismic volume into different depositional or non-depositional packages. This diagram provides better understanding on the spatial distribution of deposition through the geological time. In this paper, we will firstly introduce the GeoTime? methodology, and then demonstrate two application examples. The first example is taken at a regional scale, where GeoTime? was used to automatically track the major stratigraphic surfaces within a first order progradation system. The seismic volume was then segmented into sub order sequences bounded by the automatically tracked surfaces. 3D Wheeler diagram was also constructed to understand the depositional history. The second example is taken at reservoir scale from a producing field with more than 800 borehole penetration. In this example, we imposed geological constraint into the GeoTime? workflow, and improved the previous interpretation of higher order prograding clinoforms for placing new development wells.
机译:ChronoStraphic地震解释提供了叠加进化的见解。通过映射内部地层架构,该方法已广泛用于井放置优化和储层模型建筑。在多年的研究中,Sismage团队已经创建了地理工程?,一种用于地震数据的自动计时分析的软件工具,特别是在复杂的地质环境中。该工具可用于自动或半自动跟踪计时曲面表面。输出是地层表面的3D立方体(ISO-地质时间),可用于构建地理典的框架工作。通过将地震体积分割成不同的沉积或非沉积包装,也可以获得“轮车图”的3D立方体。该图提供了更好地了解通过地质时间沉积的空间分布。在本文中,我们首先会介绍地理工程?方法论,然后演示两个应用示例。第一个例子是以地区的区域规模拍摄的?用于在一阶促进系统中自动跟踪主要地层表面。然后将地震体积分段为由自动跟踪表面限定的亚阶序列。 3D轮式图也被构建以了解沉积历史。第二个例子是从生产领域的储液量表,具有超过800个钻孔渗透的。在这个例子中,我们将地质限制施加到地质时间?工作流程,并改进了先前对高阶促进临床植物的解释,以便在新的发展井上进行新的开发井。

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