SEG Technical Program Expanded Abstracts 2012 2012
DOI: 10.1190/segam2012-1034.1
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Stratigraphic features within the Ratawi Shale Member of the Lower Cretaceous Ratawi Formation and their hydrocarbon prospectivity in Sudaira – Abdali area, North Kuwait

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Cited by 4 publications
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“…The upper Ratawi member is also known as the Ratawi Shale member which is mainly composed of marine shale/claystone, interbedded by siltstone and fine-grained sandstone, and limestone streaks (Arasu et al, 2012). The origin of the sandstone is attributed to the uplift and erosion of the Arabian Shield (Al-Fares et al, 1998;Sharland et al, 2001).…”
Section: Ratawi Formationmentioning
confidence: 99%
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“…The upper Ratawi member is also known as the Ratawi Shale member which is mainly composed of marine shale/claystone, interbedded by siltstone and fine-grained sandstone, and limestone streaks (Arasu et al, 2012). The origin of the sandstone is attributed to the uplift and erosion of the Arabian Shield (Al-Fares et al, 1998;Sharland et al, 2001).…”
Section: Ratawi Formationmentioning
confidence: 99%
“…Major oil discoveries were found in the lower part of the Ratawi Limestone Member at Wafra and Umm Gudair fields since the 1950s. However, in the last 10 years, Kuwait Oil Company has shifted its exploration efforts to the Ratawi Shale Member where it tested oil in the Umm Gudair Field in the south, Rugae in the southwest, and Sabriyah, Raudhatain, and Abdali fields in north Kuwait (Arasu et al, 2012. And Al-Tendail et al, 2012.…”
Section: Ratawi Formationmentioning
confidence: 99%
“…The Ratawi Formation comprises siliciclastic mudstones and calcareous siliciclastic mudstones with tiny lime-mudstone intercalated with thin, muddy sandstones. The entire Ratawi Shale interval is thought to have been deposited in calm offshore circumstances with intermittent bottom current interruptions, most likely due to storms (Azim et al 2019;Arasu et al 2012). The Lower Cretaceous period recorded two transgressive-regressive cycles: the older cycle spanning Minagish and Ratawi formations and the younger cycle spanning Zubair and Shuaiba Formations (Haq and Al-Qahtani 2005;Sharland et al 2001).…”
Section: Stratigraphy and Petroleum Systemmentioning
confidence: 99%
“…The field is divided into the western Umm Gudair sector, the eastern Umm Gudair sector, and the southern Umm Gudair sector ( Figure 1 B). The Minagish Oolite/Middle member of the Minagish Formation has moderate to high porosity, is hydrocarbon-bearing, and is considered the main contributor of hydrocarbon production in the Umm Gudair Field ( Arasu et al., 2012 ). The Minagish Formation has been deposited on a broad, prograding carbonate, has a thickness range from 160 m in Burgan Field in the south to 360 m in the northern fields, and has three members.…”
Section: Introductionmentioning
confidence: 99%