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On a method for reducing interpretation uncertainty of poorly imaged seismic horizons and faults using geomechanically based restoration technique

机译:基于地质力学的还原技术减少成像差的地震层位和断层解释不确定性的方法

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摘要

To reduce exploration risk and optimize production in structurally complex areas, the geologic interpretation must be based on sound geomechanical principles. Despite advances in 3D seismic acquisition and processing techniques as well as in the availability of computationally robust interpretation software, the challenge associated with interpreting complex structures from seismic reflection data is that highly deformed areas surrounding faults, folds, and salt surfaces are often poorly imaged and therefore their interpretation is highly uncertain. We have developed a methodology that should help geophysicists quickly check the strengths and weaknesses of their interpretation and to automatically reduce the uncertainty in a faulted horizon geometry. Our workflow consisted of restoring interpreted seismic horizons and relating the concentrations of computed deformation attributes to areas of interpretation uncertainty. We used the technique based on an iterative finite-element formulation that allowed unfolding and unfaulting of 3D horizons using physical elastic behavior. A fast algorithm has been developed to automatically correct the interpreted structures in zones that exhibited anomalous deformation concentrations after restoration. This approach is able to mechanically check and reduce uncertainty in a faulted seismic horizon interpretation. Its application to synthetic and reservoir data has a high degree of reliability in the characterization of structurally complex reservoirs. This technique is also applicable to 2D models (geologic cross sections) and 3D models (volume).
机译:为了降低勘探风险并优化结构复杂区域的产量,地质解释必须以合理的地质力学原理为基础。尽管3D地震采集和处理技术取得了进步,并且具有强大的计算解释软件,但从地震反射数据解释复杂结构所面临的挑战是,断层,褶皱和盐面周围的高度变形区域的成像效果通常很差,因此,它们的解释是高度不确定的。我们已经开发出一种方法,可以帮助地球物理学家快速检查其解释的优缺点,并自动减少有缺陷的层位几何学中的不确定性。我们的工作流程包括恢复解释的地震层位并将计算出的变形属性的浓度与解释不确定性区域相关联。我们使用基于迭代有限元公式的技术,该公式允许使用物理弹性行为来展开和破坏3D层。已经开发出一种快速算法来自动校正恢复后呈现异常变形集中的区域中的解释构造。这种方法能够以机械方式检查并减少地震层位解释中的不确定性。它在合成和储层数据中的应用在表征结构复杂的储层方面具有高度的可靠性。该技术还适用于2D模型(地质剖面)和3D模型(体积)。

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