首页> 外文会议>SPWLA annual logging symposium;Society of Petrophysicists and Well Log Analysts, inc >NEW METHOD FOR ROCK CLASSIFICATION IN CARBONATE FORMATIONS USING WELL-LOG-BASED ROCK FABRIC QUANTIFICATION
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NEW METHOD FOR ROCK CLASSIFICATION IN CARBONATE FORMATIONS USING WELL-LOG-BASED ROCK FABRIC QUANTIFICATION

机译:碳酸盐岩地层岩性定量的碳酸盐岩地层分类新方法

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Inconsistencies are commonplace in identifyingpetrophysical rock classes and geological depositionalfacies in carbonate formations. Different diageneticprocesses may cause the same geological facies toexhibit different petrophysical properties. Theseinconsistencies can be overcome by quantitatively takinginto account spatial distribution of pore network and rockfabric in rock classification and petrophysicalevaluation. Mercury Injection Capillary Pressure(MICP)-based pore typing does take into account thepore structure through pore size distribution. However,such measurements are not commonly available in allwells and depth intervals of interest. Furthermore, welllog-based rock classification techniques do not take intoaccount rock fabric and require the number of rockclasses as an input parameter. There is often uncertaintyin the optimum number of rock classes, which mainlyroots in the differences between petrophysical rockclasses and the geological depositional facies. In thispaper, we introduce a method to (a) evaluate porenetwork connectivity and geometry as rock fabric usingcombined evaluation of pore- and log-scalemeasurements in each rock class, (b) improve rockclassification in carbonate formations by simultaneouslyevaluating conducting porosity, permeability, and rockclasses in the formation, and (c) optimize the number ofrock classes in the formation.
机译:不一致在识别中很常见 岩石物理分类与地质沉积 碳酸盐岩地层相。不同的成岩作用 过程可能导致相同的地质相 表现出不同的岩石物理特性。这些 不一致可以通过定量分析来克服 考虑孔隙网络和岩石的空间分布 岩石分类和岩石物理中的织物 评估。汞喷射毛细管压力 (MICP)型毛孔分型确实考虑了 通过孔径分布的孔结构。然而, 这种测量并非在所有国家中都普遍可用 感兴趣的井和深度区间。此外,welllog- 基于岩石的分类技术不考虑 核算岩石结构并要求岩石数量 类作为输入参数。经常会有不确定性 在最佳的岩石类别数量中,主要是 根源于岩石物理岩石之间的差异 类和地质沉积相。在这个 在论文中,我们介绍了一种方法(a)评估孔隙 网络连通性和几何结构,如使用 孔隙度和对数尺度的综合评估 每个岩石等级的测量,(b)改善岩石 同时进行碳酸盐岩地层分类 评估传导孔隙率,渗透率和岩石 编队,并且(c)优化数量 岩层中的地层。

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