埃及西北沙漠Abu El-Gharadig主油田上白垩统Abu Roash和Bahariya油藏特征

N. El-Gendy, M. Noweir, Mohamed S. El-Sadek, A. Ali
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引用次数: 1

摘要

研究区位于Abu El-Gharadig盆地,北纬29°40′~ 29°45′,东经28°25′~ 28°32′之间。该研究旨在评估位于埃及西北部沙漠Abu El-Gharadig盆地中部的四个地层。通过岩石物理分析,研究Abu Roash“D”和“E”段以及Bahariya组晚白垩世含油气储层。为了实现这一目标,交互式岩石物理软件(IP) 3.5版帮助进行了测井评价,提供了密度-中子和M-N交叉图,以表征储层的孔隙度和岩性,以及页岩和次生孔隙度对储层潜力的影响。此外,软件提供了模拟表明岩石物性参数的垂直分布的研究,显示页岩体积的分布,孔隙度、含水饱和度、烃饱和度和识别含油区域。岩石物性参数分析表明,Abu Roash“D”储层以灰岩为主,岩性为砂岩和页岩,而Abu Roash“E”储层以砂岩为主,岩性为页岩、灰岩和白云岩。上、下巴哈里亚地区储层以砂岩为主,含泥质和钙质胶结物。Abu Roash (D、E)段和上、下Bahariya组页岩体积分别为0.9 ~ 3.8%、8.2 ~ 13.7%、7.2 ~ 15.2%和9 ~ 15.5%,有效孔隙度分别为6.7 ~ 14.7%、13.9 ~ 18.1%、13.1 ~ 15.5%和11.4 ~ 15.5%,具有较好的储层质量。通过模拟显示Abu Roash和Bahariya储层的岩石物理数据,以确定具有良好油气潜力的最有效厚度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reservoir Characterization of the Upper Cretaceous Abu Roash and Bahariya Reservoirs, Main Abu El-Gharadig Oil Field, North Western Desert, Egypt
T HE study area is located in Abu El-Gharadig basin, between 29° 40’ and 29° 45’ N latitudes and 28° 25’ and 28° 32’ E longitudes. The study aims to evaluate four formations that are located in the middle part of Abu El-Gharadig Basin, North Western Desert, Egypt. This is carried out by conducting petrophysical analysis, to investigate the late Cretaceous hydrocarbon-bearing reservoirs of the Abu Roash “D” and “E” Members, and the Bahariya Formations. To achieve the aim, Interactive Petrophysics software (IP) version 3.5 helped in well-logging evaluation providing the density-neutron and the M-N cross_plot, to characterize the porosity and lithology of the reservoirs and the effect of shale and secondary porosity on the potentials of these reservoirs. In addition, the software presents analogs indicating the vertical distribution of petrophysical parameters for the studied well and to show the distribution of shale volume, porosity, water saturation and hydrocarbon saturation and identify the oil-bearing zones. Analysis of the petrophysical parameters report that, the Abu Roash “D” reservoir is mostly limestone with sandstone and shale lithology, while the Abu Roash “E” reservoir is primarily sandstone, with shale, limestone and dolomite lithology. The reservoirs in the Upper and Lower Bahariya are mostly sandstones, with argillaceous and calcareous types of cement. The shale volumes in the Abu Roash ( D and E ) Members and Upper and Lower Bahariya Formation are 0.9 – 3.8 %, 8.2 – 13.7, 7.2 – 15.2, and 9 – 15.5 %, respectively, and the effective porosities are 6.7 – 14.7 %, 13.9 – 18.1 %, 13.1 – 15.5 % and 11.4 – 15.5 %, expressing a good reservoir quality of the zones. Petrophysical data from the Abu Roash and Bahariya reservoirs are shown on analogs, to identify the most effective thicknesses with good hydrocarbon potential.
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