Porosity characterization of complex silicified carbonates reservoirs of BM-C-33

P. D. Luca, A. Waldum, A. S. Chandler, D. Hunt, O. P. Wennberg, G. McQuenn, D. Hulme, E. Castro, L. Loures, J. Matias, I. Søreide, A. Filgueiras
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引用次数: 2

Abstract

Summary “Block BM-C-33 sits in the SW quadrant of the Campos Basin, approximately 200km off the coast of Rio de Janeiro, Brazil. Three discoveries (Seat, Gavea and Pao de Acucar) were made between 2009 and 2012. Following appraisal, these are now believed to hold reserves of more than one billion barrels of oil equivalent. Reservoirs in Block BM-C-33 were growing in the outer Campos Basin during the Aptian. They sit on top of rotated and eroded fault blocks and paleo volcanic highs. On a regional scale, they can be viewed as a distal continuation of the Coqueiros and Macabu formations. Seismically, the accumulations are characterized by a wedge-shaped and mounded external geometry ( Hunt, et al., 2019 ). The reservoirs of BM-C-33 are unique. The original rock has been subject to a range of diagenetic processes which completely have altered the original mineral assemblage and pore textures. The resulting reservoir rock displays a complex pore network - different from what is observed in other pre-salt reservoirs. Silica is a key component in the reservoirs of BM-C-33. According to recent works ( Lapponi et al, 2019 , Tritlla et al, 2018 ; Tritlla, et al, 2019 ), the origin of the silica is both early, during or shortly after deposition; and late, associated with hydrothermal activity most likely in Mid Albian ( Tritlla et al, 2018 ). Pore types are diverse and pores range in size from micro porosity to meter scale caverns. Measurements of permeability at different scales reflect this diversity. Permeability measurements on SWC’s capture matrix properties and are generally low (a few mD and below). DST’s on the other hand suggest average reservoir scale permeabilities of several hundreds of mD. Frequent and occasionally massive mud losses during drilling of reservoir sections confirm the presence of large-scale pore systems. Reservoir properties in carbonate reservoirs are closely tied to pore types. NMR and BHI (BoreHole Image) logs are keys for typing of matrix and larger scale pores respectively. Lack of whole core and production logs make conceptual models important but alternative scenarios are carried forward to capture the uncertainty span. Characterization of reservoir properties in BM-C-33 depends on multidisciplinary work and integration of data on a wide range of scales. Whilst the matrix holds most of the hydrocarbon in place, excess permeability features as fractures, faults, connected vugs and caverns control flow. This abstract discusses some key features and the work that has been done to characterize them.”
BM-C-33复杂硅化碳酸盐岩储层孔隙度表征
BM-C-33区块位于Campos盆地的西南象限,距离巴西里约热内卢海岸约200公里。2009年至2012年间发现了三个新发现(Seat、Gavea和Pao de Acucar)。经过评估,这些油田现在被认为拥有超过10亿桶石油当量的储量。BM-C-33区块的储层在Aptian时期在Campos盆地外围发育。它们位于旋转侵蚀的断块和古火山高地之上。在区域范围内,它们可以被视为Coqueiros和Macabu地层的远端延续。从地震角度看,储层具有楔形和丘状的外部几何形状(Hunt等,2019)。BM-C-33油藏是独一无二的。原始岩石经历了一系列成岩作用,完全改变了原始矿物组合和孔隙结构。由此产生的储层岩石显示出复杂的孔隙网络,这与在其他盐下储层中观察到的不同。二氧化硅是BM-C-33储层的关键成分。根据最近的研究(Lapponi et al, 2019, Tritlla et al, 2018;Tritlla等人,2019),二氧化硅的起源既在沉积早期,也在沉积期间或沉积后不久;晚,与热液活动最有可能在中Albian (Tritlla et al, 2018)。孔隙类型多样,孔隙大小从微孔到米级溶洞不等。不同尺度的渗透率测量反映了这种多样性。SWC捕获基质性质的渗透率测量值通常较低(几个mD以下)。另一方面,DST表明平均储层渗透率为数百mD。在钻井过程中,储层段频繁出现大量泥浆漏失,证实了大规模孔隙系统的存在。碳酸盐岩储层的储层性质与孔隙类型密切相关。核磁共振测井和钻孔成像测井分别是划分基质和大尺度孔隙类型的关键。由于缺少整个岩心和生产日志,概念模型非常重要,但为了捕获不确定性范围,可以采用替代方案。BM-C-33储层性质的表征取决于多学科工作和大范围数据的整合。虽然基质将大部分碳氢化合物保持在原位,但过度渗透率以裂缝、断层、连通的孔洞和洞穴为特征,控制着流动。这篇摘要讨论了一些关键特征和已经做的工作来表征它们。
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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