Overcoming Coring Challenges in a New Unconventional Play Offshore by Integration of Formation Evaluation Data

T. Bradley, P. H. Fjeld, Jonathan Scott, S. Ogilvie
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引用次数: 1

Abstract

A well was drilled into a prospective new unconventional mudstone play offshore Norway. Two of five coring runs were successful while the rest yielded little to no core recovery. Investigations attributed the poor recovery to sub-optimal coring practices, equipment failure and operational errors. Recently, the accompanying petrophysical logs and seismic data were revisited, and upon detailed investigation several unusual responses were observed to correspond with intervals of poor core recovery. Subsequent investigation of the core itself substantiated that the coring issues largely had natural causes. This understanding is being applied to two imminent coring operations and has driven selection of drilling, coring and wireline technology and procedures, in addition to informing casing design. Wireline nuclear magnetic resonance (NMR) and cross dipole acoustic data, logging whilst drilling (LWD) density (including azimuthal images), neutron porosity and resistivity was acquired over the interval of interest for standard formation evaluation purposes. This interpretation was conducted immediately after the initial drilling and showed the formation to be a series of highly porous oil bearing mudstones. However, no in depth advanced interpretation was conducted at the time. Recently, advanced analysis including high resolution log enhancement, NMR 2D porosity and saturation analysis, acoustic azimuthal anisotropy, near wellbore imaging, fracture interpretation, and borehole image interpretation were performed on the log data, and new and improved 3D seismic data was interpreted. When interpreted in detail it could be observed that unusual responses in the logs showed a close correspondence to the intervals of poor core recovery. In particular, high azimuthal anisotropy was observed, and when this was compared to the near wellbore reflection image a significant planar reflecting feature was identified which is determined to be a fault. Indications of this feature was subsequently found in seismic data. When then compared to the azimuthal density image after resolution enhancement was applied, although the image is still of too low resolution to directly image the fault, disturbed bedding was observed which is commonly associated with faulted intervals. Several core fragments proved to have extensive small-scale fracturing not noticed previously, and slickenlines were found along several larger fractures previously presumed to be drilling induced. The investigations of the log data revealed that a previously unknown sub-seismic fault was present right below the depth where coring problems were encountered. The detailed interpretation was able to determine the precise location of the fault and its extent in the formation. Knowledge of this subsequently explained the coring problems encountered and helps to optimise imminent coring in the same formation. Lessons learned and the methodology likely also applies to similar formations. In this paper we discuss coring issues encountered in a new and unconventional play offshore, present new data and interpretation that sheds light on them and describe the methodology of the detailed integrated interpretation that uncovered the previously unknown root cause. We then discuss how these findings can be (and are) used to optimise both drilling, coring, and logging operations in future wells.
整合地层评价数据,克服海上非常规油藏取心挑战
在挪威海上一个有发展前景的非常规泥岩区钻了一口井。五次取心中有两次是成功的,而其余的取心几乎没有恢复。调查将采收率低归因于取心不佳、设备故障和操作错误。最近,对随附的岩石物理测井和地震数据进行了重新研究,经过详细调查,观察到一些不寻常的响应与岩心采收率较低的区间相对应。随后对岩心本身的调查证实,岩心问题在很大程度上是自然原因造成的。这一认识被应用于即将进行的两次取心作业,并推动了钻井、取心和电缆技术和程序的选择,此外还为套管设计提供了信息。电缆核磁共振(NMR)和交叉偶极子声学数据、随钻测井(LWD)密度(包括方位角图像)、中子孔隙度和电阻率数据在感兴趣的层段内获得,用于标准地层评价。这种解释是在首次钻井后立即进行的,并表明该地层是一系列高孔隙含油泥岩。然而,当时没有进行深入的高级解释。最近,对测井数据进行了高分辨率测井增强、核磁共振二维孔隙度和饱和度分析、声波方位各向异性、近井成像、裂缝解释和井眼图像解释等高级分析,并对新的和改进的三维地震数据进行了解释。当详细解释时,可以观察到,日志中的异常响应与岩心采收率差的间隔密切对应。特别是观察到高方位各向异性,当将其与近井反射图像进行比较时,发现了一个明显的平面反射特征,这被确定为断层。随后在地震资料中发现了这一特征的迹象。与增强后的方位角密度图像进行对比,虽然图像的分辨率仍然太低,无法直接显示断层,但可以观察到断层层序的扰动,这通常与断层层序有关。一些岩心碎片被证明存在以前没有注意到的广泛的小规模裂缝,并且在以前认为是钻井引起的几个较大裂缝沿线发现了滑溜线。对测井数据的调查显示,在遇到取心问题的深度正下方存在一个以前未知的次地震断层。详细的解释能够确定断层的精确位置及其在地层中的范围。了解了这一点之后,可以解释遇到的取心问题,并有助于优化同一地层的即将取心。经验教训和方法可能也适用于类似的地层。在本文中,我们讨论了在海上一个新的非常规油藏中遇到的取心问题,提供了新的数据和解释,阐明了这些问题,并描述了详细的综合解释方法,揭示了以前未知的根本原因。然后,我们讨论了如何利用这些发现来优化未来井的钻井、取心和测井作业。
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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