2019
DOI: 10.1016/j.jafrearsci.2019.04.015
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Pore and fracture pressure modeling using direct and indirect methods in Badri Field, Gulf of Suez, Egypt

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Cited by 76 publications
(51 citation statements)
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“…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). Hermina et al (1989) Abdelghany et al 2020;Radwan 2020a, b, c;Radwan et al 2020a, b).…”
Section: Lithostratigraphy and Geologic Settingmentioning
confidence: 99%
“…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). Hermina et al (1989) Abdelghany et al 2020;Radwan 2020a, b, c;Radwan et al 2020a, b).…”
Section: Lithostratigraphy and Geologic Settingmentioning
confidence: 99%
“…where (H) syn is the fitting density for the shallow section, R S is the surface sediment density (with a default value of 1.90 g/ cm 3 , based on the Gulf of Mexico), TVD is the true vertical depth, AG is air gas, is the exponent coefficient (default value: 0.6, for Gulf of Mexico), and all depths in the equation are in feet. 25 3.3 | Injection/fall-off tests and in situ stress measurement Injection/fall-off is a single transient test of well pressure, which is suitable for high-and low-pressure reservoirs, and is the most commonly used well testing method in CBM wells (Figure 3). In this test, water is injected into the well for a period of time with a relatively stable displacement and an injection pressure lower than the fracture pressure of the coal seam, and is then the well is closed, such that the pressure and the original reservoir pressure tend to gradually become balanced.…”
Section: Density Loggingmentioning
confidence: 99%
“…2). These fields are located in a tilted fault-block setting, which formed during middle to late Miocene rifting (Radwan et al 2019b(Radwan et al , 2020a. With a throw of 460 m at the top of middle Miocene strata, an Edipping extensional fault bounds the field to the east and separates the Badri field from the adjacent East Badri field (Fig.…”
Section: Geological Background and Tectonic Settingmentioning
confidence: 99%