Integrated petrophysical, sedimentological and well-log study of the Mangahewa Formation, Taranaki Basin, New Zealand

Dk Nurulnazihah Pg Norsahminan, Md Aminul Islam, Surya Tejasvi Thota, Mohamed Ragab Shalaby
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Abstract

This study aims to address the problem of porosity preservation in the Mangahewa Formation of five main hydrocarbon fields covering onshore and offshore of the Taranaki Basin. An integrated reservoir characterization of the Middle to Late Eocene Mangahewa Formation is achieved through petrophysical evaluation, sedimentological and petrographical descriptions, and well log analysis methods. Petrophysical parameters (porosity and permeability) were acquired from the available core analysis and using mathematical equations to obtain other petrophysical matrices such as normalized porosity index (NPI) and reservoir quality index (RQI). Factors that affected Mangahewa reservoir were studied through thin-section microscopy and well-log analysis helped to measure the reservoir and hydrocarbon potentiality in the Mangahewa Formation. The Mangahewa Formation is dominated by sandstone and a range of marginal to shallow marine facies with varying hydraulic flow units (HFU). The Mangahewa Formation has a high positive correlation in porosity-permeability relationship and has a maximum of 4.67 μm RQI and 20.08 μm FZI (Well Kapuni-14) which reflect potential reservoir. The Mangahewa Formation observed from Wells Kapuni-14, Maui-A1G, McKee-16A, and Mokau-1 are dominated with 59.6%, 56.4%, 79.3%, and 68% of macro- and megapores, respectively. The presence of authigenic clay and calcite cement has greatly reduced the reservoir quality; however, primary and secondary pores are still observed within the Mangahewa sands. Moreover, well log analysis was carried out on four wells in Taranaki Basin, to run a qualitative and quantitative analysis of the Mangahewa reservoir. Eight potential reservoir zones were examined, revealing that the Mangahewa Formation has a very low shale volume of less than 6%, good effective porosity ranging between 11.0% and 13.3%, up to 36.2% of average water saturation and maximum of 69.8% average hydrocarbon saturation. In conclusion, from this comprehensive study, it can be deduced that the Mangahewa Formation possesses fair to good reservoir quality and hydrocarbon potentiality.

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新西兰塔拉纳基盆地曼加赫瓦地层岩石物理、沉积学和测井记录综合研究
本研究旨在解决塔拉纳基盆地陆上和近海五个主要油气田曼加赫瓦地层的孔隙度保存问题。通过岩石物理评价、沉积学和岩石学描述以及测井分析方法,对中更新世至晚更新世曼加赫瓦地层进行了综合储层特征描述。岩石物理参数(孔隙度和渗透率)是通过现有岩心分析获得的,并利用数学公式获得其他岩石物理矩阵,如归一化孔隙度指数(NPI)和储层质量指数(RQI)。通过薄片显微镜和井记录分析研究了影响曼加赫瓦储层的因素,有助于测量曼加赫瓦地层的储层和碳氢化合物潜力。曼加赫瓦地层主要由砂岩和一系列边缘至浅海层组成,水流单元(HFU)各不相同。曼加赫瓦地层的孔隙度-渗透率关系呈高度正相关,最大 RQI 为 4.67 μm,FZI 为 20.08 μm(卡普尼-14 号井),反映了潜在的储层。从 Kapuni-14、Maui-A1G、McKee-16A 和 Mokau-1 号井观察到的曼加赫瓦地层中,巨型和巨型聚合物分别占 59.6%、56.4%、79.3% 和 68%。自生粘土和方解石胶结物的存在大大降低了储层质量,但在曼加赫瓦砂岩中仍可观察到原生和次生孔隙。此外,还对塔拉纳基盆地的四口油井进行了测井分析,以对曼加赫瓦储油层进行定性和定量分析。对八个潜在储层区进行了研究,结果表明,曼加赫瓦地层的页岩体积非常小,小于 6%,有效孔隙率在 11.0% 至 13.3% 之间,平均含水饱和度高达 36.2%,平均碳氢化合物饱和度最高达 69.8%。总之,从这项综合研究中可以推断出,曼加赫瓦地层具有一般到良好的储层质量和碳氢化合物潜力。
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