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Lithologic characterization of the Barnett Shale: Controls on reservoir quality.

机译:巴内特页岩的岩性特征:储层质量控制。

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摘要

The overall objective of this study was to determine the lithologic controls on reservoir quality in the Barnett Shale and to build depositional and sequence stratigraphic models to predict reservoir quality.;Core analysis led to the definition of four main lithofacies; siliceous mudstone, argillaceous mudstone, calcareous mudstone, and dolomitic mudstone. Each lithofacies effectively represents an end member of the quartz-carbonate-clay ternary diagram. The lithofacies show a mixture of detrital and authigenic constituents that each correlate to a specific depositional environment.;The siliceous mudstone facies was found to be the highest quality reservoir facies. Siliceous mudstones are characterized by the highest porosity and permeability in the Barnett as well as the most efficient fabric for the formation and preservation of primary interparticle porosity. A byproduct of this semi-rigid framework is brittleness, which makes the siliceous mudstone the best facies to land a horizontal well and propagate hydraulic fractures.;The vertical distribution of TOC is a function of production, destruction, and concentration/dilution of organic matter. The three variables and the relationships among them are tied to depositional environments and the unique conditions that produce them.;Analysis of lithofacies led to the recognition of a series of depositional environments associated with sedimentation on an oxygen-deficient continental shelf. The depositional environments were characterized by the position of sea level and the resulting effects on sedimentation and geochemistry. The cyclical pattern of rising and falling sea level led to deposition of stacked packages that can be quantified and predicted by applying a sequence stratigraphic model.;It was shown that sequence stratigraphic subdivisions, such as possible 3nd-order sequence boundaries, can be inferred by the utilization of basinwide cross sections that provided data that cannot be seen with one core. These basin scale trends could be combined with higher resolution reservoir analysis similar to this one to create very effective reservoir quality prediction models.
机译:这项研究的总体目标是确定Barnett页岩储层质量的岩性控制,并建立沉积和层序地层学模型以预测储层质量。硅质泥岩,泥质泥岩,钙质泥岩和白云质泥岩。每个岩相有效地代表了石英-碳酸盐-粘土三元图的末端。岩相显示出碎屑和自生成分的混合物,每种都与特定的沉积环境有关。硅质泥岩相被认为是质量最高的储层相。硅质泥岩的特征是巴尼特(Barnett)的孔隙率和渗透率最高,并且是形成和保留主要颗粒间孔隙率的最有效织物。这种半刚性框架的副产品是脆性,这使硅质泥岩成为沉积水平井并传播水力压裂的最佳相。; TOC的垂直分布是有机物的产生,破坏和浓缩/稀释的函数。这三个变量及其之间的关系与沉积环境和产生它们的独特条件有关。岩相分析导致人们认识到一系列与缺氧大陆架上的沉积有关的沉积环境。沉积环境的特征是海平面的位置及其对沉积和地球化学的影响。海平面上升和下降的周期性模式导致堆积包裹的沉积,这些堆积包裹可以通过应用层序地层学模型来量化和预测。研究表明,层序地层细分(例如可能的三阶层序边界)可以通过利用流域范围内的横截面提供了一个岩心无法看到的数据。这些流域规模趋势可以与与此类似的高分辨率储层分析相结合,以创建非常有效的储层质量预测模型。

著录项

  • 作者

    Miller, Brett.;

  • 作者单位

    Oklahoma State University.;

  • 授予单位 Oklahoma State University.;
  • 学科 Geology.;Geochemistry.
  • 学位 M.S.
  • 年度 2014
  • 页码 123 p.
  • 总页数 123
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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