Noreen Kausar, Azeem Tahir, Rehman Faisal, Amin Yawar, Ahmad Qazi Adnan, Hussain Mureed
Department of Earth Sciences, Quaid-i- Azam University, Islamabad, Pakistan.
College of Energy and Mining Engineering, Shandong University of Science and Technology, Qingdao, China.
PLoS One. 2025 May 22;20(5):e0324793. doi: 10.1371/journal.pone.0324793. eCollection 2025.
The reservoir quality of the Lower Goru Formation is highly variable due to its heterogeneous nature influenced by sea level fluctuations during the Early Cretaceous period. This study applies an unsupervised machine learning workflow, integrating Principal Component Analysis (PCA) for dimensionality reduction, Self-Organizing Maps (SOM) for clustering, and fuzzy classification for geological labeling, alongside petrophysical evaluation and cross-plot analysis, to assess the impact of clay minerals on the reservoir quality of the Lower Goru Formation in the NIM-Tay block, Lower Indus Basin, Pakistan. Petrophysical analysis delineates a potential reservoir zone (1455-1517 m) characterized by 13.9% effective porosity and 27.3% water saturation. The first four principal components explain approximately 90% of the dataset variance. Electrofacies classification distinguishes four facies-Impermeable Reservoir, Potential Reservoir, Non-Reservoir, and Tight Reservoir-each corresponding to specific clay mineral assemblages. Cross-plot and electrofacies analysis reveal that facies dominated by chlorite and montmorillonite preserve porosity (15%) and permeability (888.87 mD), whereas kaolinite-rich and mixed-layer clay facies significantly reduce reservoir quality. This study provides a reproducible and scalable framework for integrating machine learning with petrophysical workflows, offering improved reservoir characterization not only in the Lower Indus Basin but also in similar heterogeneous sandstone reservoirs globally.
由于受早白垩世海平面波动影响,下戈鲁组储层性质不均一,储层质量变化很大。本研究应用一种无监督机器学习工作流程,结合主成分分析(PCA)进行降维、自组织映射(SOM)进行聚类以及模糊分类进行地质标注,同时进行岩石物理评价和交会图分析,以评估粘土矿物对巴基斯坦印度河下游盆地NIM-Tay区块下戈鲁组储层质量的影响。岩石物理分析划定了一个潜在储层带(1455 - 1517米),其有效孔隙度为13.9%,含水饱和度为27.3%。前四个主成分解释了约90%的数据集方差。电相分类区分出四个相——不透水储层、潜在储层、非储层和致密储层——每个相都对应特定的粘土矿物组合。交会图和电相分析表明,以绿泥石和蒙脱石为主的相保持了孔隙度(15%)和渗透率(888.87毫达西),而富含高岭石和混合层粘土的相显著降低了储层质量。本研究为将机器学习与岩石物理工作流程相结合提供了一个可重复且可扩展的框架,不仅为印度河下游盆地,也为全球类似的非均质性砂岩储层提供了改进的储层表征。