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    川东北地区二叠系大隆组页岩岩石物理建模及横波预测研究

    Rock physical properties and modeling of Permian Dalong shales in northeastern Sichuan Basin

    • 摘要: 川东北地区二叠系大隆组页岩属于典型的海相页岩储层,具备良好的页岩气勘探开发潜力。然而,当前针对该优质储层岩石物理规律的系统性研究不够深入,导致储层甜点预测缺乏坚实的物理依据。为此,开展了系统的页岩样品岩石学特征、储层特征及岩石物理测试与分析,结合微观结构特征,基于自相容近似(SCA)模型与微分等效介质(DEM)模型,引入多重孔隙结构假设,构建了适用于该研究区的岩石物理模型及解释量版。研究结果表明,大隆组主要发育硅质、混合质及灰质等页岩,储层矿物组分呈高硅质矿物含量、高碳酸盐矿物占比、低黏土矿物含量的显著特征,其岩石物理弹性响应表现为孔隙度高、总有机质(TOC)含量高、波速低以及各向异性弱等特性。利用岩心实验数据对所建岩石物理模型进行验证,结果表明预测结果与岩心实验数据吻合度较高;进一步将该模型应用于研究区大隆组页岩储层的测井横波速度预测,预测结果与实际测井数据匹配度达到85%,为川东北地区大隆组页岩储层的甜点预测提供了可靠的理论依据与技术支撑。

       

      Abstract: The shales in the Permian Dalong Formation in the northeastern Sichuan Basin represent typical high-quality marine reservoirs with substantial potential for shale gas exploration and development. However, systematic experimental studies on their rock physical properties remain insufficient, resulting in a lack of solid petrophysical basis for sweet-spot prediction. To address this, our study focuses on the systematic lab testing and analysis of the petrological, reservoir, and rock physical characteristics of the shale samples from the study area. By integrating with the microstructural observations and incorporating a multi-porosity hypothesis, a rock physical model, and corresponding interpretation templates, is established based on the self-consistent approximation and differential effective medium model. The results indicate that Dalong shales mainly comprise siliceous, mixed, and calcareous shales. The mineral composition is characterized by high silica content, high carbonate content, and low clay content. The rock physical responses present high porosity, high total organic carbon (TOC) content, low wave velocity, and weak anisotropy. The model-based calculations show high consistency with core data. The model-based shear velocity predictions demonstrate an 85% match with measured log data, providing a reliable theoretical foundation and technical support for seismic sweet-spot prediction in Permian Dalong shales in northeastern Sichuan Basin.

       

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