Evaluating Complex Lacustrine Carbonate Reservoir by Integrating Advanced Logging Techniques and Core Measurements-A Case Study in Qiadam Basin

Wen An Chen, D. Yu, Guoyan Liu, Qing Bo Li, Diqiu Zhang, Meng Zhao, Fang fang Wu, Liang Cai, Xianran Zhao, Shenzhuan Li, J. Wu
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Abstract

A complex and tight lacustrine carbonate reservoir is the main target reservoir in Qaidam Basin. The diagenesis of shallow-shore lake deposition has created a highly heterogeneous reservoir in both vertical and horizontal directions in terms of lithologies, pore structures, and permeability. The core analysis shows a wide variety of lithologies that include terrigenous clastics (quartz, orthoclase, and plagioclase), carbonate (calcite, dolomite, and ankerite), and evaporite minerals such as anhydrite, etc. Electron microscope analysis shows mainly intercrystallite pores with dolomite, dissolved pores, and microfractures. Associated with the complex lithology and pore structure, reservoir permeability is varied and is mostly less than 0.02mD. Evaluating and characterizing this complex reservoir to find a better pay zone was the objective of this study. To evaluate the lithologies, pore structures, porosities, and permeability in quantities accurately, the advanced gamma-ray spectroscopy logs, nuclear magnetic resonance (NMR) logs, and high-resolution micro-resistivity borehole image logs were acquired in some key wells. Integrated with core data such as X-ray diffraction (XRD), mercury injection capillary (MICP), the lithofacies, texture facies, and pore facies were classified based on the minerals from gamma-ray spectroscopy, the textures from borehole image, and the pore sizes from NMR. The combination of these three facies represents the reservoir quality. In the study area, the lithofacies were classified into four types, which are high carbonate content facies, middle carbonate content facies, high clay content facies, and high clastic content facies. The texture facies were classified into four types, which are massive texture, layered texture, dissolved texture, and algal texture. The pore structure facies were classified into four types, which are macro facies, meso facies, meso-micro facies, and microfacies. The better pay zone is the combination of high carbonate content facies, algal texture, and macro facies. The pay zone of the reservoir was well defined and mapped with the combination facies vertically and horizontally in the whole study area. The integrated solution described in this study leverages the advantages of advanced gamma-ray spectroscopy, NMR, borehole images, and core measurements. It develops a comprehensive understanding of the complex carbonate reservoir and provides the solution to pinpoint the sweet spots and place the horizontal well.
先进测井技术与岩心测量相结合评价复杂湖相碳酸盐岩储层——以塔里木盆地为例
复杂致密的湖相碳酸盐岩储层是柴达木盆地的主要目标储层。浅滩湖沉积的成岩作用形成了一个在岩性、孔隙结构和渗透率方面在垂直和水平方向上都高度非均质的储层。岩心分析显示出多种岩性,包括陆源碎屑(石英、正长石和斜长石)、碳酸盐(方解石、白云石和铁白云石)和蒸发岩矿物(硬石膏等)。电镜分析显示主要为晶间孔隙、白云岩孔隙、溶蚀孔隙和微裂缝。由于储层岩性和孔隙结构复杂,储层渗透率变化较大,大多小于0.02mD。对该复杂储层进行评价和表征,寻找更好的产层是本研究的目的。为准确定量评价岩性、孔隙结构、孔隙度和渗透率,对部分重点井进行了先进的伽玛能谱测井、核磁共振测井和高分辨率微电阻率井眼成像测井。结合x射线衍射(XRD)、注汞毛细管(MICP)等岩心数据,根据伽玛能谱矿物、井眼图像结构和核磁共振孔径对岩心岩相、结构相和孔隙相进行了分类。这三种相的组合代表了储层的物性。研究区岩相可划分为高碳酸盐含量相、中碳酸盐含量相、高粘土含量相和高碎屑含量相4种类型。将构造相划分为块状、层状、溶解和藻状4种类型。将孔隙结构相划分为宏观相、中观相、中微相和微相4种类型。较好的产层为高碳酸盐相、藻质相和宏观相的组合。在整个研究区进行了油藏产层圈定,并在纵向和横向上进行了组合相圈定。本研究中描述的集成解决方案利用了先进的伽马射线光谱、核磁共振、井眼图像和岩心测量的优势。它对复杂的碳酸盐岩储层有了全面的了解,并提供了精确定位甜点和水平井位置的解决方案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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