2020
DOI: 10.1016/j.jafrearsci.2019.103746
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Thermal maturity modelling for the pre-Miocene source rocks in Ras Garra area, Suez rift Basin, Egypt

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Cited by 4 publications
(3 citation statements)
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“…Page|64 Smale et al 1988 [36] ; Burchette 1988 [37] ; Richardson and Arthur 1988 [38]; Abd El Shafy 1990 [39]; Darwish 1992 [40]; Hughes et al 1992 [41]; Rouchy et al 1995 [42]; Darwish and El-Araby, 1993 [43]; Alsharhan and Salah 1994 [5], 1995 [44], 1997 [45]; Plaziat et al 1998 [46]; Bosence et al 1998 [47]; Salah and Alsharhan, 1998 [48]; Peijs et al 2012 [49]; Rohais et al 2016 [50]; Elmaadawy, 2020 [51]).…”
Section: Geologic and Tectonic Frameworkmentioning
confidence: 99%
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“…Page|64 Smale et al 1988 [36] ; Burchette 1988 [37] ; Richardson and Arthur 1988 [38]; Abd El Shafy 1990 [39]; Darwish 1992 [40]; Hughes et al 1992 [41]; Rouchy et al 1995 [42]; Darwish and El-Araby, 1993 [43]; Alsharhan and Salah 1994 [5], 1995 [44], 1997 [45]; Plaziat et al 1998 [46]; Bosence et al 1998 [47]; Salah and Alsharhan, 1998 [48]; Peijs et al 2012 [49]; Rohais et al 2016 [50]; Elmaadawy, 2020 [51]).…”
Section: Geologic and Tectonic Frameworkmentioning
confidence: 99%
“…Tectonic subsidence occurred at a high rate in the deposition of the Upper Rudeis (160 m / Ma) and Lower Rudeis (435 m / Ma) formations during the rift. After these episodes of high tectonic subsidence well Sinai-1, the stage of early mature of the pre-Miocene source rocks started at 14.60 Ma, and in GM-A1 well, the Lower Rudeis rock started the stage of early mature at 15.53 Ma (Elmaadawy, 2020 [51]).…”
Section: The Development Of the Petroleum System In Garra Regionmentioning
confidence: 99%
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