REAL-TIME 2.5D INVERSION OF LWD RESISTIVITY MEASUREMENTS USING DEEP LEARNING FOR GEOSTEERING APPLICATIONS ACROSS FAULTED FORMATIONS

K. Noh, C. Torres‐Verdín, D. Pardo
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引用次数: 3

Abstract

We develop a Deep Learning (DL) inversion method for the interpretation of 2.5-dimensional (2.5D) borehole resistivity measurements that requires negligible online computational costs. The method is successfully verified with the inversion of triaxial LWD resistivity measurements acquired across faulted and anisotropic formations. Our DL inversion workflow employs four independent DL architectures. The first one identifies the type of geological structure among several predefined types. Subsequently, the second, third, and fourth architectures estimate the corresponding spatial resistivity distributions that are parameterized (1) without the crossings of bed boundaries or fault plane, (2) with the crossing of a bed boundary but without the crossing of a fault plane, and (3) with the crossing of the fault plane, respectively. Each DL architecture employs convolutional layers and is trained with synthetic data obtained from an accurate high-order, mesh-adaptive finite-element forward numerical simulator. Numerical results confirm the importance of using multi-component resistivity measurements -specifically cross-coupling resistivity components- for the successful reconstruction of 2.5D resistivity distributions adjacent to the well trajectory. The feasibility and effectiveness of the developed inversion workflow is assessed with two synthetic examples inspired by actual field measurements. Results confirm that the proposed DL method successfully reconstructs 2.5D resistivity distributions, location and dip angles of bed boundaries, and the location of the fault plane, and is therefore reliable for real-time well geosteering applications.
利用深度学习技术实现LWD电阻率测量的实时2.5d反演,用于断层地层的地质导向应用
我们开发了一种深度学习(DL)反演方法,用于解释2.5维(2.5D)井眼电阻率测量结果,该方法的在线计算成本可以忽略不计。通过对断层和各向异性地层的三轴随钻电阻率测量数据的反演,成功地验证了该方法。我们的深度学习反演工作流采用了四个独立的深度学习架构。第一种方法在几种预定义类型中识别地质构造的类型。随后,第二、第三和第四种结构分别估算了参数化后的电阻率空间分布,分别为(1)不跨越床界或断裂面,(2)跨越床界但不跨越断裂面,(3)跨越断裂面。每个深度学习架构都采用卷积层,并使用从精确的高阶网格自适应有限元正演数值模拟器获得的合成数据进行训练。数值结果证实了使用多分量电阻率测量(特别是交叉耦合电阻率分量)对于成功重建井眼轨迹附近的2.5D电阻率分布的重要性。结合现场实际测量的两个综合算例,对开发的反演工作流程的可行性和有效性进行了评价。结果证实,该方法成功地重建了2.5D电阻率分布、层界位置和倾角以及断平面位置,因此可用于实时井地导向应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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