Naturally Fractured Zone Identification – A Multi Attribute Deepwater Gulf of Mexico Example

H. Andrade, P. Bt-Mokhta, A. B-Zulkifli
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Abstract

Summary Direct fracture detection using surface seismic data is challenging due to seismic resolution, signal-to-noise ratio, structural setting and rock properties among many others causes. The ability to detect sub-seismic faults and fracture rich zones on the seismic image requires advanced workflows. The result of being able to identify small fault and fractures enables optimal well path designs and de-risking of target locations. This presentation will demonstrate a multi-attribute workflow which includes volumetric curvature parameter optimization, directional GLCM (gray-level co-occurrence matrix) based attributes, and post processing enhancement with 3D Log-Gabor filtering. Comparison between volumetric curvature and texture classification based on GLCM is carried out in order to get an estimation of fracture corridor orientations. An array of sectors response from GLCM-based attributes can be calculated in different directions by inspecting and comparing these different sectors. Areas with clear tendency to directional variations might be associated with fractured zones, changes in lithology, or seismic facies changes. Based on these analyzes it was possible to identify highly fractured zones congruous with the geological model. The main trend shows parallelism with the main faults and a secondary is interpreted as a direct expression of the salt influence. These observations are consistent with modeled anticline generated by salt tectonics and limited by main sealing faults. This methodology was used to predict the fractured zones on top of the Cretaceous brecciated carbonates in the Gulf of Mexico that are the most important reservoirs in the Salinas Basin.
天然裂缝带识别——以墨西哥湾深水多属性为例
由于地震分辨率、信噪比、构造环境和岩石性质等诸多因素的影响,使用地面地震数据进行直接裂缝检测具有挑战性。在地震图像上检测次地震断层和裂缝丰富带的能力需要先进的工作流程。能够识别小断层和裂缝的结果可以优化井眼轨迹设计并降低目标位置的风险。本演讲将演示一个多属性工作流,其中包括体积曲率参数优化,基于定向GLCM(灰度共生矩阵)的属性,以及3D Log-Gabor滤波的后处理增强。将基于GLCM的体积曲率和纹理分类方法进行比较,得到裂缝走廊方向的估计。通过检查和比较这些不同的部门,可以从不同的方向计算出基于glcm的属性的一系列部门响应。方向性变化趋势明显的地区可能与裂缝带、岩性变化或地震相变化有关。基于这些分析,可以识别出与地质模型一致的高裂缝带。主走向与主断裂平行,次走向是盐作用的直接表现。这些观测结果与盐构造产生的模拟背斜一致,并受到主要封闭断层的限制。该方法被用于预测墨西哥湾白垩纪角砾岩顶部的裂缝带,这些裂缝带是萨利纳斯盆地最重要的储层。
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