Assessment of the petrophysical properties and hydrocarbon potential of the Lower Miocene Nukhul Formation in the Abu Rudeis-Sidri Field, Gulf of Suez Basin, Egypt

Lower Miocene rift sediments of the Nukhul Formation are one of the prominent hydrocarbon producers in the Gulf of Suez basin. In this study, we focused on the oil producing Nukhul sandstones of the Abu Rudeis-Sidri Field, located in the east central Gulf of Suez. Nukhul Formation is characterized b...

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Veröffentlicht in:Geomechanics and geophysics for geo-energy and geo-resources. 2023-12, Vol.9 (1), Article 36
Hauptverfasser: Farouk, Sherif, Sen, Souvik, Belal, Nancy, Omran, Mohammad A., Assal, Ehab M., Sarhan, Mohammad A.
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container_title Geomechanics and geophysics for geo-energy and geo-resources.
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creator Farouk, Sherif
Sen, Souvik
Belal, Nancy
Omran, Mohammad A.
Assal, Ehab M.
Sarhan, Mohammad A.
description Lower Miocene rift sediments of the Nukhul Formation are one of the prominent hydrocarbon producers in the Gulf of Suez basin. In this study, we focused on the oil producing Nukhul sandstones of the Abu Rudeis-Sidri Field, located in the east central Gulf of Suez. Nukhul Formation is characterized by the prominent low amplitude seismic reflectors and represents the youngest identified reflector (Lower Miocene) in the study area. Petrophysical assessment was carried out using wireline logs to infer the reservoir characteristics. The Nukhul sandstone reservoir exhibits lower shale volume (
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The calculated water saturation of the reservoir zone in the three productive wells ranges between 0.17 and 0.34 dec (i.e., the hydrocarbon saturation equals 0.66–0.87 dec). A small range of bulk volume of water (0.011–0.03 dec) indicates superior quality of the hydrocarbon-bearing sandstone intervals. Absence of productive sands in one of the studied wells, drilled in the hanging wall implied structural control on hydrocarbon accumulation in the study area. This study provides crucial insights regarding the quantitative petrophysical characteristics, reservoir quality distribution and hydrocarbon potential of the Lower Miocene Nukhul clastic reservoir. Highlights This study presents the quantitative petrophysical characterization of the Lower Miocene Nukhul sandstones. The reservoir sandstones are calcareous in nature and consist of montmorillonite as the dominant clay phase. 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Geophys. Geo-energ. Geo-resour</stitle><date>2023-12-01</date><risdate>2023</risdate><volume>9</volume><issue>1</issue><artnum>36</artnum><issn>2363-8419</issn><eissn>2363-8427</eissn><abstract>Lower Miocene rift sediments of the Nukhul Formation are one of the prominent hydrocarbon producers in the Gulf of Suez basin. In this study, we focused on the oil producing Nukhul sandstones of the Abu Rudeis-Sidri Field, located in the east central Gulf of Suez. Nukhul Formation is characterized by the prominent low amplitude seismic reflectors and represents the youngest identified reflector (Lower Miocene) in the study area. Petrophysical assessment was carried out using wireline logs to infer the reservoir characteristics. The Nukhul sandstone reservoir exhibits lower shale volume (&lt; 0.1 dec dominantly), 0.07–0.16 dec total porosity and effective porosity up to 0.13 dec within the Nukhul sandstone interval. Bulk density-neutron porosity cross plot infers primarily sandstone matrix with the influence of carbonates, which characterizes the studied reservoir as calcareous sandstones. Spectral gamma ray data indicates montmorillonite as the principal clay phase along with minor kaolinite and illite. The calculated water saturation of the reservoir zone in the three productive wells ranges between 0.17 and 0.34 dec (i.e., the hydrocarbon saturation equals 0.66–0.87 dec). A small range of bulk volume of water (0.011–0.03 dec) indicates superior quality of the hydrocarbon-bearing sandstone intervals. Absence of productive sands in one of the studied wells, drilled in the hanging wall implied structural control on hydrocarbon accumulation in the study area. This study provides crucial insights regarding the quantitative petrophysical characteristics, reservoir quality distribution and hydrocarbon potential of the Lower Miocene Nukhul clastic reservoir. Highlights This study presents the quantitative petrophysical characterization of the Lower Miocene Nukhul sandstones. The reservoir sandstones are calcareous in nature and consist of montmorillonite as the dominant clay phase. Reservoir exhibits very high hydrocarbon saturation with high lateral variations in porosity and shale volume.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s40948-023-00572-w</doi><oa>free_for_read</oa></addata></record>
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subjects Bulk density
Carbonates
Clay
Effective porosity
Energy
Engineering
Environmental Science and Engineering
Foundations
Gamma rays
Geoengineering
Geophysics/Geodesy
Geotechnical Engineering & Applied Earth Sciences
Hanging walls
Hydraulics
Hydrocarbons
Illite
Illites
Kaolinite
Miocene
Montmorillonite
Montmorillonites
Oil and gas exploration
Oil exploration
Porosity
Reflectors
Reservoirs
Sandstone
Saturation
Sedimentary rocks
Sediments
Shale
Shales
title Assessment of the petrophysical properties and hydrocarbon potential of the Lower Miocene Nukhul Formation in the Abu Rudeis-Sidri Field, Gulf of Suez Basin, Egypt
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