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首页> 外文期刊>AAPG Bulletin >Bioturbation influence on reservoir quality: A case study from the Cretaceous Ben Nevis Formation, Jeanne d'Arc Basin, offshore Newfoundland, Canada
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Bioturbation influence on reservoir quality: A case study from the Cretaceous Ben Nevis Formation, Jeanne d'Arc Basin, offshore Newfoundland, Canada

机译:生物扰动对储层质量的影响:以加拿大纽芬兰近海的珍妮·达克盆地白垩纪本尼维斯组为例

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摘要

The delineation Ben Nevis L-55 well, located in the Hebron-Ben Nevis field, offshore Newfoundland, targeted the Cretaceous Ben Nevis Formation in the petroleum-rich Jeanne d'Arc Basin. This case study focuses on the bioturbated net-pay horizons and assesses the importance of animal-sediment interactions in controlling the porosity and permeability of sandstone reservoir intervals. Our data reveal that bioturbation can either reduce permeability and porosity by as much as approximately 33% or enhance it by up to 600%, dependent on burrow type and behavior of the trace-making organism. The net-pay interval in the cored interval of Ben Nevis L-55 is characterized by Ophiomorpha-dominated ichnofabrics. The action of bioturbators can be classified in terms of sediment mixing, sediment cleaning, sediment packing, and pipe-work-building strategies. Bioturbation has the potential to increase isotropy or uniformity of grain size by destroying sedimentary laminae through burrow homogenization, or decrease isotropy by selectively sorting grains into burrow lining and fill by grain size, and through creation of open-burrow systems filled with later sediments of differing character to the host sediment. The petrophysical characteristics of the reservoir facies are highly dependent on trace fossil morphology, presence or absence of burrow linings, nature of burrow fills, burrow size, and bioturbation intensity. Mudstone-rich facies and ichno-fabrics containing mudstone-filled and/or lined burrows (e.g., Ophiomorpha and clusters of Chondrites) have the net effect of permeability reduction. In contrast, permeability enhancement is documented from muddy sandstone facies with clean sand-filled burrows (e.g., Thalassinoides) and clean sandstones with burrow-mottled or diffuse to massive textures.
机译:本·尼维斯L-55井的轮廓位于纽芬兰近海的希伯伦-本尼维斯油田,目标是石油资源丰富的珍妮·德Arc盆地的白垩纪本·尼维斯地层。该案例研究的重点是生物扰动的净产值范围,并评估了动物-沉积物相互作用在控制砂岩储层孔隙度和渗透率中的重要性。我们的数据表明,取决于洞穴类型和造迹生物的行为,生物扰动可以使渗透率和孔隙率降低多达约33%,也可以使渗透率和孔隙率提高多达600%。本尼维斯L-55核芯间隔中的净薪金间隔的特征在于,以麦田为主导的鱼眼织物。生物扰动器的作用可以根据泥沙混合,泥沙清洁,泥沙堆积和管道施工策略进行分类。生物扰动有可能通过挖洞均质化破坏沉积层来增加各向同性或粒度的均匀性,或通过有选择地将谷粒分类到挖洞衬里并按粒度填充,以及通过创建开放式挖洞系统来填充各向后的不同沉积物来降低各向同性。寄主沉积物的特性。储层相的岩石物理特征高度依赖于痕迹化石形态,是否存在洞穴衬里,洞穴填充物的性质,洞穴大小和生物扰动强度。富含泥岩充填和/或衬砌的洞穴(例如麦冬和球粒陨石簇)的富泥岩相和鱼类纤维具有降低渗透率的净效果。相比之下,渗透性增强是由具有干净的充满沙子的洞穴(例如Thalassinoides)的泥质砂岩相和具有斑驳的或散布到块状纹理的干净的砂岩记录的。

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