Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data
Zahra, H., Nakhla, A. (2015). Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data. EKB Journal Management System, 4(1), 64-85. doi: 10.1016/j.nrjag.2015.04.003
Hesham Shaker Zahra; Adel Mokhles Nakhla. "Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data". EKB Journal Management System, 4, 1, 2015, 64-85. doi: 10.1016/j.nrjag.2015.04.003
Zahra, H., Nakhla, A. (2015). 'Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data', EKB Journal Management System, 4(1), pp. 64-85. doi: 10.1016/j.nrjag.2015.04.003
Zahra, H., Nakhla, A. Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data. EKB Journal Management System, 2015; 4(1): 64-85. doi: 10.1016/j.nrjag.2015.04.003

Deducing the subsurface geological conditions and structural framework of the NE Gulf of Suez area, using 2-D and 3-D seismic data

NRIAG Journal of Astronomy and Geophysics
Volume 4, Issue 1, June 2015, Pages 64-85    PDF (14.11 M)
DOI: 10.1016/j.nrjag.2015.04.003
Authors
Hesham Shaker Zahra; Adel Mokhles Nakhla
Abstract
An interpretation of the seismic data of Ras Budran and Abu Zenima oil fields, northern central Gulf of Suez, is carried out to evaluate its subsurface tectonic setting. The structural configuration, as well as the tectonic features of the concerned area is criticized through the study of 2D and 3D seismic data interpretation with the available geological data, in which the geo-seismic depth maps for the main interesting levels (Kareem, Nukhul, Matulla, Raha and Nubia Formations) are depicted. Such maps reflect that, the Miocene structure of Ras Budran area is a nearly NE–SW trending anticlinal feature, which broken into several panels by a set of NWSE and NE–SW trending faults. The Pre-Miocene structure of the studied area is very complex, where Ras Budran area consists of step faults down stepping to the south and southwest, which have been subjected to cross faults of NE–SW trend with lateral and vertical displacements.
Keywords
Seismic data; Ras Budran and Abu Zenima oil fields; Study of 2D and 3D seismic data; Step faults
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