建立全碳酸盐岩储层关系:基于孔喉的岩石分型网络

Jamari M Shah, Nur Athirah Md Dahlan, Hazreen Harris Lee, Nur Fatihah M Zulkifli
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引用次数: 0

摘要

碳酸盐岩储层非均质性高于碎屑岩储层,碎屑岩储层相对仅受沉积相控制。这是由于纵向和横向上的相变化比较强烈,成岩作用也比较强烈。因此,需要一种精确的方法来确保油气开发的有效性和效率。碳酸盐表征的挑战与岩石类型和孔隙度有关。岩石的渗透率不能仅由孔隙度来决定。确定岩石类型和估计岩石渗透率的方法是通过岩石分型法。该方法适用于因成岩作用而发生动态变化的碳酸盐岩储层。认为可以较好地预测和优化碳酸盐岩储层。岩心资料可以根据岩石相的地质特征或电相表征的岩石物理特征来确定岩石类型,岩石分型方法有基于形状和趋势的孔喉组、PGS -孔隙几何结构、Lucia、FZI -流带指示、Winland R35等。这些方法采用不同的原理来划分岩石类型。主要目的将基于地质陈述信息的岩心结果与数字化工程数据进行合并。通过结合这两部分信息和数据,可以更精确地求解岩石类型,并能够实现对碳酸盐岩储层更精细的表征。此外,还对台地碳酸盐岩、尖顶碳酸盐岩和复杂碳酸盐岩岩性等多种碳酸盐岩环境进行了分析。本文通过基于孔喉的岩石分型,提出了主要考虑地质和工程因素的碳酸盐岩环境岩石分型方法。主要的岩石分型组可以由地层或孔喉的分布形状来确定。这将产生所有样品的孔隙度-渗透率关系。然后使用地质输入来描述更精细和详细的关系特征。这些不同的数据集将有助于填充整个油藏的地质特征和每一层的深度。该过程包括开发孔喉大小与孔喉连通性网络之间的相关性。根据岩心塞孔喉模式和测井响应进行定义。因此,通过多口测井曲线之间的相关性,在非取心层段中传播。将讨论一些关键的岩石物理测量,以及如何解释与碳酸盐有关的钻孔图像。此外,我们还研究了不同的岩石分类方法,以及建立静态碳酸盐岩模型的最佳实践。该方法是利用孔喉组对碳酸盐岩储层岩石类型进行分类。主要的岩石分型组可以由地层或孔喉的分布形状来确定。该方法必须首先在有芯层段进行测试。考虑到碳酸盐结构的复杂性,这是为了确保纳入了足够的数据。这将产生所有样品的孔隙度-渗透率关系。然后使用地质输入来描述更精细和详细的关系特征。钻后岩心塞的分析通常来自沉积学分析、薄片、SEM、XRD甚至岩心照片。这些不同的数据集将有助于填充整个油藏的地质特征和每一层的深度。这些步骤将有助于重新聚集孔隙度-渗透率关系。在执行这些步骤之后,将在采用方法之前对输出进行校准,并回归到未取芯的区间。利用该方法进行的基于孔喉群的渗透率预测与岩心渗透率实测值吻合,捕捉到了渗透率变化的复杂响应。结果表明,利用储层孔喉分布可以进行岩石分型。这是因为用这种方法填充的渗透率反映了储层的复杂性。通过创建基于孔喉的岩石类型,结果更加详细。这进一步得到所有可用地质数据的支持和结合。台地型、尖顶型和复杂碳酸盐岩之间存在显著差异。该工作流程集成了关键信息,以进一步捕获复杂的碳酸盐岩储层系统。这种方法是一种新颖的方法,应推广到世界上其他碳酸盐岩储层,使我们对复杂的碳酸盐岩储层结构或网络有更多的了解。这项研究是可靠的,能够捕获多种碳酸盐环境,并与世界各地的几个盆地进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Establishing Rapport Throughout Carbonate Reservoirs: A Rock Typing Networking Based on Pore Throat
Carbonates reservoir has an elevated level of heterogeneity than clastic reservoir, which is relatively controlled only by depositional facies. It is because of the facies variation vertically and laterally which is more intensive, as well as intensive diagenesis. Therefore, an accurate method is required to ensure hydrocarbon development is effective and efficient. Challenges in the characterization of the carbonate are related to rock type and porosity. The permeability of rocks cannot to determined only by porosity. The method that can be used to determine rock type and rock permeability estimation is through rock typing method. This method is aptly applied for carbonate reservoir which is dynamically change due to diagenesis. It is believed to predict and optimize carbonate reservoir better. Core data can be used to determine rock type based on geology named litho-facies or petrophysics named electro-facies characterization There are many rock typing methods, which are Pore throat group based on shape and trend, PGS - Pore geometry structure, Lucia, FZI – flow zone indicator, Winland R35. Those methods use different principles in classifying rock type. Main objective to merge core results between geological statement information based with digital engineering data. By combining these two pieces of information and data, the more precise rock type and able to achieve in solving more finer on carbonate reservoir characterization. Furthermore, the analysis has been conducted over multiple carbonates environments including platform carbonate, pinnacle carbonate and complex carbonate lithology. This paper presents the rock typing classification in carbonate environments which consider geological, and engineering elements mainly through Pore Throat based Rock typing. The main rock typing group can be derived from either stratigraphy or the distribution shape of the pore throat. This will produce the porosity-permeability relationship for all the samples. Geological inputs are then used to describe more refined and detailed characteristics of the relationship. These variety sets of data will help to populate the geological features of the reservoir in bulk and each individual layer in depths. The process includes developing the correlation between pore throat size and pore throat connectivity networking. Defined from core plug pore throat pattern and tie to well logs respond. Consequently, to be propagated in the non-cored intervals through correlation between multiple well logs respond. Some of the key petrophysical measurements will be discussed and how to interpret the borehole images associated with carbonates. As well as looking at different methods of rock typing and best practices to build a static carbonate model. This approach is using pore throat group to classify the rock typing of the carbonate reservoirs. The main rock typing group can be derived from either stratigraphy or the distribution shape of the pore throat. The methodology must be tested first in cored intervals. This is to ensure that sufficient data has been incorporated considering the complexity of the carbonate structure. This will produce the porosity-permeability relationship for all the samples. Geological inputs are then used to describe more refined and detailed characteristics of the relationship. Post drill analysis of the core plugs usually come from the sedimentology analysis, thin section, SEM, XRD and even the core photos. These variety sets of data will help to populate the geological features of the reservoir in bulk and each individual layer in depths. These will be the steps that will aid in re-clustering the porosity-permeability relationship. After these steps have been implemented, the outputs will be calibrated before the methodology will be adopted and regressed to the un-cored intervals. The permeability prediction based on pore throat group by using this methodology matches with measured core permeability with capture the complex respond of permeability variation. The result shows rock typing can be generated by using the pore throat distribution of the reservoirs. This is because permeability populated by this method captures the complexity of the reservoir. Results are more detailed by creating rock typing based on the pore throat. This is furthermore supported and incorporated with all available geological data. There is a significant difference that can be seen between platform, pinnacle, and complex carbonate. The workflow integrates critical information to further capture the complex carbonate reservoir system. This kind of approach is novel and should be adopted to the other carbonate reservoirs in the world for us to understand more on complicated carbonate reservoir structures or network. This study is robust and able to capture multiple carbonate environments and in comparison, with several basins from various parts of the world.
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