2015
DOI: 10.1016/j.jafrearsci.2015.05.020
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Petrophysical analysis and hydrocarbon potentialities of the untested Middle Miocene Sidri and Baba sandstone of Belayim Formation, Badri field, Gulf of Suez, Egypt

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Cited by 47 publications
(34 citation statements)
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“…The stratigraphic units in the Gulf of Suez can be subdivided into three mega sediment groups (Fig. 2): (1) the Cambrian-Oligocene pre-rift sequence; (2) the Oligocene-Miocene syn-rift sequence (the core of the present study), which comprises the main hydrocarbon reservoirs as well as seals in the Gulf of Suez (Nukhul, Rudies, Kareem, Belayim, South Gharib, Zeit, and post-Zeit seals and reservoir rocks); and (3) the post-rift post-Miocene mega-sequence (Bosworth and McClay 2001;Attia et al 2015;Nabawy and El Sharawy 2015;Abudeif et al 2016aAbudeif et al , 2016bAbudeif et al , 2018; Radwan Egypt (EGPC 1996). et al 2019b, 2020aKassem et al 2021).…”
Section: Lithostratigraphy and Geologic Settingmentioning
confidence: 96%
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“…The stratigraphic units in the Gulf of Suez can be subdivided into three mega sediment groups (Fig. 2): (1) the Cambrian-Oligocene pre-rift sequence; (2) the Oligocene-Miocene syn-rift sequence (the core of the present study), which comprises the main hydrocarbon reservoirs as well as seals in the Gulf of Suez (Nukhul, Rudies, Kareem, Belayim, South Gharib, Zeit, and post-Zeit seals and reservoir rocks); and (3) the post-rift post-Miocene mega-sequence (Bosworth and McClay 2001;Attia et al 2015;Nabawy and El Sharawy 2015;Abudeif et al 2016aAbudeif et al , 2016bAbudeif et al , 2018; Radwan Egypt (EGPC 1996). et al 2019b, 2020aKassem et al 2021).…”
Section: Lithostratigraphy and Geologic Settingmentioning
confidence: 96%
“…The Middle to Upper Serravallian Belayim Formation, which is the most important syn-rift oil reservoirs, is unconformably underlain by the Kareem Formation and its contact with the overlying South Gharib Formation is a disconformity. The Belayim Formation shows very good hydrocarbon accumulations within its sandstone interbeds (Richardson and Arthur 1988;EGPC 1996;Al-sharhan 2003;Attia et al 2015;Nabawy and Barakat 2017;Radwan and Sen 2020). The Belayim Formation is composed of four members, the Hammam Faraun (top of Belayim Formation), Feiran, Sidri, and Baba (base of Belayim Formation).…”
Section: Lithostratigraphy and Geologic Settingmentioning
confidence: 99%
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“…Different parts of the Gulf of Suez have different geological histories. The succession, facies changes and the relationships of the different blocks that comprise the Gulf of Suez are quite variable so that no single area in the Gulf is found to be wholly representative of the stratigraphy or the structure of the entire region (Said 1962;Steen and Helmy 1982 The generalised litho-stratigraphic column within the North Ramadan oil field shown in (Figure 2), for which three depositional phases are generally assumed (Attia et al 2015).…”
Section: Geologic Settingmentioning
confidence: 99%
“…It is an intra-continental, late Oligocene rifted basin but was originally formed during the early Palaeozoic as a narrow embayment of the Tethys that was intensively rejuvenated during the rifting phase of the great East African rift system in the Palaeocene. (Abudeif et al, 2016;Bosworth and McClay 2001;Lashin and Abd El-Aal 2004;D'Agosto et al 2008;Abd El-Naby et al 2010;Attia et al 2015) It can be described as a rejuvenated, slightly accurate NW-SE trending rifted graben, which separates the shield of central Sinai from that of the Eastern Desert of Egypt and extends from latitude 27°15ʹ to 30°N and 32°10ʹ to 34°E embracing a total length of 350 km with average width ranging between 30 and 80 km, and average water depth of 160 ft.…”
Section: Introductionmentioning
confidence: 99%