碳酸盐岩台地环境下通道化体系的表征——以伊拉克超大型油田晚白垩世储层为例

A. Al-Ali, K. Stephen, Asghar Shams
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摘要

潮汐通道通道的识别是预测突水风险较高区域行为的关键,对油藏开发和动态监测具有重要影响。然而,碳酸盐岩中的潮汐通道通常不容易用常规地震属性来表征。综合多源数据和多种方法,对破解碳酸盐岩潮道构型的复杂性具有重要意义。本文对测井资料进行了岩石学特征和岩相分析,并用岩心资料进行了仔细验证。然后,第二步是将巴哈马潮滩和Wadi Mi'Aidin(阿曼北部)的露头尺度的碳酸盐水道系统与现代类似物进行比较。然后,采用监督概率神经网络(PNN)和线性回归方法检测额外的通道分布。高孔隙度与低声阻抗的关系多出现在河道相,反映了良好的储层质量。在这些通道外,岩石被潮旁碳酸盐岩严重泥质充填,具有高声阻抗异常和低孔隙分布质量的特征。PNN孔隙体积的新观测揭示了Mishrif碳酸盐岩潮汐通道在古潮流方向和连通性方面的横向分布。此外,岩心资料的先验信息和地质知识与分类岩性具有较好的一致性。这些观测结果表明,由于沉积环境的影响,Mishrif水道具有广泛的岩性和孔隙型波动。这项工作使我们对河道体的分布和岩石物性有了新的认识,并量化了它们对主要生产储层动态储层行为的影响。这项工作不仅将为本案例的开发和生产提供重要的指导,而且还将为伊拉克南部附近油田类似的地质和沉积环境提供综合的工作路径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterization of Channelized Systems in a Carbonate Platform Setting: A Case Study on the Late Cretaceous Reservoir from the Supergiant Oilfield, Iraq
Identification of tidal channels fairways is key for predicting behavior of areas at higher risk to water breakthrough or otherwise have a significant impact on the development and monitoring of reservoir performance. However, tidal channels in carbonates are not often easily characterized using conventional seismic attributes. It is important to decipher the complexity of the carbonate tidal channel architecture with integrated multisource data and a variety of approaches. In this paper, petrological characteristics and petrographic analysis is conducted on well logs and validated carefully using core data. Then, the second step is to compare the carbonate channel systems with modern analogue in Bahama tidal flat and outcrop scales in Wadi Mi'Aidin (Northern Oman). Thereafter, the supervised probabilistic neural network (PNN) and linear regression method were undertaken to detect an additional channel distribution. The relationship of high porosity with low acoustic impedance appeared mostly in the channel facies which reflects good reservoir quality grainstone channels. Outside these channels, the rock is heavily mud filled by peritidal carbonates and characterized by a high acoustic impedance anomaly with low quality of porosity distribution. The new observation of PNN porosity volume revealed a lateral distribution of the Mishrif carbonate tidal channels in terms of paleocurrent direction and the connectivity. Additionally, the prior information from core data and the geological knowledge indicate a good consistency with classified lithology. These observations implied that Mishrif channels consist of a wide range of lithology and porotype fluctuations due to the impact of depositional environment. The work enables us to provide a new insight into the distribution of channel bodies, and petrophysical properties with quantification of their influence on dynamic reservoir behavior of the main producing reservoir. This work will not only provide an important guidance to the development and production of this case study, however also deliver an integrated work path for the similar geological and sedimentary environment in the nearby oil fields of Southern Iraq.
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