首页> 外文会议>SPWLA Annual Logging Symposium >INTEGRATED MULTI-PHYSICS WORKFLOW FOR AUTOMATIC ROCK CLASSIFICATION AND FORMATION EVALUATION USING MULTI-SCALE IMAGE ANALYSIS AND CONVENTIONAL WELL LOGS
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INTEGRATED MULTI-PHYSICS WORKFLOW FOR AUTOMATIC ROCK CLASSIFICATION AND FORMATION EVALUATION USING MULTI-SCALE IMAGE ANALYSIS AND CONVENTIONAL WELL LOGS

机译:使用多尺度图像分析和传统井日志的自动摇滚分类和形成评估集成多物理工作流程

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Conventional well-log-based rock classification often overlooks rock fabric features (spatial distribution of solid and fluid rock components), which makes it not comparable against geologic facies, especially in formations with complex rock fabric. This challenge is usually addressed by identification of geological facies from core description and their integration with measured petrophysical properties. However, manual identification of geological facies using core data is a tedious and time-consuming process. In this paper, we propose an automatic workflow for joint interpretation of conventional well logs, computed tomography (CT) scan/core images, and routine core analysis (RCA) data for simultaneously optimizing rock classification and formation evaluation. First, we perform conventional well-log interpretation to obtain petrophysical properties of the evaluated depth intervals. Subsequently, we automatically extract rock-fabric related features derived from core photos and core CT-Scan images. Then, we use a clustering algorithm to obtain rock classes from the extracted rock-fabric features. We optimize the number of rock classes by iteratively increasing the number of rock classes from an initially assumed number until a permeability-based cost function converges below a predefined threshold. The proposed workflow can help expedite the process of geological facies classification by providing an overview of different lithologies and an overall stacking pattern. We successfully applied the proposed workflow to a sedimentary sequence with vertically variable rock fabric and lithology. Dual energy acquired core CT-Scan images were available along with core photos, RCA data, and conventional well logs. Image-based integrated rock classes were in agreement with the lithologies encountered in the evaluated depth interval. Class-byclass permeability models improved permeability estimates by 78% (decrease in mean relative error) in comparison to formation-by-formation permeability estimates. Furthermore, rock classes were consistently propagated to another well where core and CT-Scan images were not employed for rock classification. The detected rock classes were in agreement with lithofacies obtained from core description. Permeability estimates were also in good agreement with available RCA data.
机译:传统的基于良好的基于​​良好的岩石分类通常俯视岩石织物特征(固体和流体岩石成分的空间分布),这使得与地质面不相当,特别是在具有复杂岩石织物的形成中。这一挑战通常通过鉴定来自核心描述的地质面及其与测量的岩石物理性质的整合来解决。然而,使用核心数据的地质相的手动识别是一种繁琐且耗时的过程。在本文中,我们提出了一种自动工作流程,用于传统井日志,计算机断层扫描(CT)扫描/核心图像的联合解释,以及用于同时优化Rock分类和形成评估的常规核心分析(RCA)数据。首先,我们进行传统的良好良好的良好解释,以获得评估深度间隔的岩石物理特性。随后,我们自动提取源自核心照片和核心CT扫描图像的摇滚结构相关的特征。然后,我们使用聚类算法从提取的岩石结构特征获取Rock类。通过迭代地增加来自最初假设的数字的岩石类的数量来优化岩石类的数量,直到基于渗透率的成本函数收敛在低于预定阈值下方。拟议的工作流程可以通过提供不同岩性和整体堆叠模式来帮助加快地质面分类的过程。我们成功将建议的工作流程应用于沉积序列,垂直变量岩石面料和岩性。双能量获取的核心CT扫描图像以及核心照片,RCA数据和传统井日志可用。基于图像的集成摇滚类与评估深度间隔中遇到的岩性一致。与形成逐个渗透率估计相比,类逐个渗透率模型提高了78%(平均相对误差的减少)。此外,岩石类始终如一地传播到另一个核心和CT扫描图像未用于岩石分类。检测到的岩石类与从核心描述中获得的锂缺失一致。渗透率估计也与可用的RCA数据吻合良好。

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