Impact of Reservoir Heterogeneity on Bitumen Content in the Mackay River Oil Sands, Athabasca (Canada)

IF 3.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Acta Geologica Sinica ‐ English Edition Pub Date : 2023-10-28 DOI:10.1111/1755-6724.15123
Xiaofa YANG, Diyun YU, Suwei WU, Junhao REN, Dingsheng CHENG, Jixin HUANG, Chengyu YANG, Guoqing MA, Meijun LI
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Abstract

The Lower Cretaceous Manville Group of Upper McMurray Formation is one of the main bitumen reservoirs in Athabasca. In this study, the relationship between reservoirs heterogeneity and bitumen geochemical characteristics were analyzed through core and microscopic observation, lab analysis, petrophysics and logging data. Based on the sedimentology framework, the formation environment of high-quality oil sand reservoirs and their significance for development were discussed. The results indicate that four types lithofacies were recognized in the Upper McMurray Formation based on their depositional characteristics. Each lithofacies reservoirs has unique physical properties, and is subject to varying degrees of degradation, resulting in diversity of bitumen content and geochemical composition. The tidal bar (TB) or tidal channel (TC) facies reservoir have excellent physical properties, which are evaluated as gas or water intervals due to strong degradation. The reservoir of sand bar (SB) facies was evaluated as oil intervals, due to its poor physical properties and weak degradation. The reservoir of mixed flat (MF) facies is composed of sand intercalated with laminated shale, which is evaluated as poor oil intervals due to its poor connectivity. The shale content in oil sand reservoir is very important for the reservoir physical properties and bitumen degradation degree. In the context of regional biodegradation, oil sand reservoirs with good physical properties will suffer from strong degradation, while oil sand reservoirs with relatively poor physical properties are more conducive to the bitumen preservation.

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储层异质性对加拿大阿萨巴斯卡麦凯河油砂沥青含量的影响
上麦克默里地层的下白垩统曼维尔组是阿萨巴斯卡地区的主要沥青储层之一。本研究通过岩心和显微观察、实验室分析、岩石物理和测井数据,分析了储层异质性与沥青地球化学特征之间的关系。在沉积学框架的基础上,讨论了优质油砂储层的形成环境及其对开发的意义。研究结果表明,根据沉积特征,在上麦克默里地层中发现了四种岩性。每种岩性储层都具有独特的物理特性,并受到不同程度的降解,导致沥青含量和地球化学成分的多样性。潮间带(TB)或潮汐通道(TC)岩相储层具有极佳的物理性质,由于降解强烈,被评价为气层或水层。沙洲(SB)面储层的物理性质较差,降解程度较弱,因此被评估为油层。混合平(MF)面储层由夹有层状页岩的砂组成,由于其连通性较差,被评估为贫油层。油砂储层中的页岩含量对储层物理性质和沥青降解程度非常重要。在区域生物降解的背景下,物理性质好的油砂储层降解程度强,而物理性质相对较差的油砂储层更有利于沥青的保存。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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