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Exploratory plays of Pará-Maranh?o and Barreirinhas basins in deep and ultra-deep waters, Brazilian Equatorial Margin

机译:巴西赤道边缘深水和超深水区的Pará-Maranh?o和Barreirinhas盆地的勘探活动

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The Pará-Maranh?o and Barreirinhas are exploratory frontier basins. After the discoveries in deep/ultra-deep water turbidites at the correlated African equatorial margin and French Guiana (Jubilee and Zaedyus plays), the exploratory interest was retaked for those basins. Using 2D seismic interpretation, it was search to identify hydrocarbon accumulations potential focusing on turbiditic reservoirs. Three plays types linked to three margin distinct segments were identified: shallow waters, faulted shelf border and deep/ultra-deep waters. The shallow waters and faulted shelf border plays are related to two petroleum systems: Caju-Travosas and Travosas-Travosas. The Caju Group (Late Albian-Early Cenomanian) and Travosas Formation (Cenomanian-Turonian) source rocks occur between 2,400 and 3,700 m below sea water bottom for shallow waters play, and between 1,300 and 4,800 m for faulted shelf border play. The deep/ultra-deep waters play is related to three petroleum systems: Codó-Travosas, Caju-Travosas and Travosas-Travosas. The source rocks from Codó Formation (Aptian) occur between 2,860 and 4,550 m, from Caju Group (Late Albian-Early Cenomanian) between 2,200 and 3,800 m and from Travosas Formation (Cenomanian-Turonian) between 1,430 and 2,860 m. In the African equatorial margin, the oil window top is located around 2,700 m below sea water bottom. Thus, it can be concluded that Pará-Maranh?o and Barreirinhas source rocks would also be able to generate oil/gas in the specified depths.
机译:Pará-Maranh?o和Barreirinhas是探索性边境盆地。在相关的非洲赤道边缘和法属圭亚那(Jubilee和Zaedyus油田)发现了深/超深水混浊物之后,这些盆地重新引起了人们的探索兴趣。使用2D地震解释,人们正在寻找以湍流储层为中心的油气聚集潜力。确定了与三个边缘不同段相关的三种游乐类型:浅水区,断层架边界和深/超深水区。浅水区和断裂的陆架边界层与两种石油系统有关:Caju-Travosas和Travosas-Travosas。 Caju组(晚阿尔拜-早西诺曼期)和Travosas组(西诺曼尼亚-突厥人)烃源岩发生在浅水区海床以下2,400至3,700 m之间,而断层架边界处在1,300至4,800 m之间。深层/超深层水域与三种石油系统有关:科多-特拉沃萨斯,卡朱-特拉沃萨斯和特拉沃萨斯-特拉沃萨斯。源于Codó组(Aptian)的岩石发生在2,860至4,550 m之间,来自Caju组(Late Albian-Early Cenomanian的岩石)发生在2,200至3,800 m之间,来自Travosas组(Cenomanian-Turonian的岩石)发生在1,430至2860 m之间。在非洲赤道边缘,油窗顶部位于海水底部下方约2700 m。因此,可以得出结论,Pará-Maranh?o和Barreirinhas的烃源岩也将能够在指定的深度产生油气。

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