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Applications of geophysical techniques to evaluate deep formations at Asala-Samra oil field, East Bahariya, Egypt

机译:地球物理技术在评估埃及东巴哈里亚Asala-Samra油田深层地层中的应用

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Using the available seismic data, this study aimed at the evaluation of the prospectivity and hydrocarbon potentialities to the deep formations structure of the Asala-Samra area.The Asala-Samra area is located in the Western Desert of Egypt, south of the Northeast Abu Gharadig Concession and west of Qarun oil field. The 3D-Seismic data covers about (56 km~2) which called East Bahariya Area. The acquisition of high quality 3D seismic data integrated with the well data resulted in accurate delineation of the structure traps and the different elements of the petroleum system in the study area. The interpretation results of the high quality seismic data contributed to in the understanding of the tectonic history of the study area. Evidences for the presence of Jurassic-Early Cretaceous rifting, Late Cretaceous rifting, Late Cretaceous-Early Tertiary inversion, and Late Tertiary (Miocene) rifting tectonics were documented from the interpretation of the seismic data. The main productive reservoirs of the study area are Abo Roash "G" member and Upper part of Bahariya Formation. This research focused on the deeper formations and structures from Early Cretaceous and Late Jurassic which didn't test as HC trap yet and aims to add new undiscovered zones. Many seismic leads of Early Cretaceous and Late Jurassic were recognized from interpreted seismic data. Most of them are four way dip closure to avoid the side sealing problem. The source rocks are working in the eastern part of the Abu Gharadig Basin. The regional top seals for the different reservoirs in the study area were evaluated through isopach maps. A reservoir evaluation of the Alam Elbueib and Safa sands has been also attempted.
机译:利用现有的地震数据,本研究旨在评估Asala-Samra地区深层构造的前景和油气潜力.Asala-Samra地区位于埃及的西部沙漠,阿布加拉迪格东北部以南特许权和卡伦油田以西。 3D地震数据覆盖了大约56 km〜2,称为东巴哈里亚地区。采集高质量的3D地震数据并结合油井数据,可以对研究区内的构造圈闭和石油系统的不同元素进行准确的描绘。高质量地震数据的解释结果有助于理解研究区的构造历史。通过地震数据的解释,记录了侏罗纪-早白垩世裂谷,晚白垩世裂谷,晚白垩世-早第三纪逆转和晚第三纪(中新世)裂陷构造的证据。研究区的主要生产储层是阿博·罗斯(Abo Roash)的“ G”成员和巴哈利亚组的上部。这项研究的重点是早白垩纪和晚侏罗世的较深地层和构造,尚未作为HC圈闭进行测试,目的是增加新的未发现带。从解释的地震数据中可以识别出早白垩纪和侏罗纪晚期的许多地震导线。它们中的大多数为四向浸入式密封,以避免侧面密封问题。烃源岩在阿布格哈拉迪格盆地东部工作。通过等渗线图评估了研究区内不同储层的区域顶盖。还尝试了对Alam Elbueib和Safa砂岩进行储层评估。

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