时间深度转换中故障定位不确定性的集成

F. Geffroy, Pedro Correia, H. Binet, J. Chautru, D. Renard, N. Nosjea-Gorgeu
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引用次数: 1

摘要

摘要断层是根据地震资料解释的物体,通常难以描述其特征。不仅断层的类型会根据建模者工作的领域(时间或深度)而有所不同,而且精确的形状映射通常会延伸到相干地震数据的水平以下。当我们考虑到断层网络表征中的简单错误可能会使地下模型在其流动特性方面无效,并提供错误的储量值时,这一点尤为重要。然而,在缺乏适当技术的情况下,深度转换工作流程不能考虑断层的不确定性,而是依赖于单一的确定性解释。本文提出了一种考虑时间深度转换工作流程中位置故障不确定性的新方法。通过考虑断层的不同实现方式,目标表面可以动态地适应这个新的位置,并可用于更新进一步的体积计算。所提出的方法可以完全自动化,并且可以更完整地探索断层解释的不确定性空间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Integration of Fault Location Uncertainty in Time to Depth Conversion
Summary Faults are objects interpreted from seismic data that are often difficult to characterize. Not only the type of a fault can appear different depending on the domain the modeler is working on (time or depth), but accurate shape mapping often extends below the level of coherent seismic data. This proves especially impactful when we consider that simple errors in the fault-network characterization can render a subsurface model useless in terms of its flow properties and provide erroneous values for volumes of reserves. Nevertheless, in absence of proper technology, depth conversion workflows do not account for fault uncertainties, instead relying on a single deterministic interpretation. This paper presents a new methodology that considers positional fault uncertainty in time-to-depth conversion workflows. By considering different realizations of a fault, the target surface is dynamically adapted to this new position and can be used to update further volumetric computations. The proposed methodology can be fully automated and results in a more complete exploration of the uncertainty space regarding fault interpretation.
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