Tectonic and basin evolution of South Eastern Mediterranean for hydrocarbon potentiality in North Sinai, Egypt
Abd-Allah, A.M.; Ahmed Abd El-Naby; Mohamed H. Abdel Aal;
Abstract
South Eastern Mediterranean margin has expressed two Jurassic-Recent tectonic cycles that related to the
opening and closure of the Neotethys Ocean. Structural and sedimentological complications related to these
cycles and the basin evolution are selected to be the main targets of the present study in North Sinai. 2D seismic,
boreholes, and outcrop data are used to achieve these targets. The development of the margin began by the
formation of the NE and E-W oriented normal faults during the Jurassic-Early Cretaceous rifting. Two Albian
uplifting phases occurred by the end of this rifting and followed by the Cenomanian-Oligocene positive inversion
that was interrupted by a tectonic loading subsidence phase allowed the deposition of the pelagic Campanian-
Maastrichtian chalk on the shallow Upper Cretaceous carbonate. Shortening related to this inversion inverted
completely the normal-slip on some rift-related faults into reverse faults and related folds or partially inverted by
decreasing of the normal slip on the others. Inversion was ended by the post-Oligocene extensional-subsidence
event that is related to north-sinking of the northern part of the African margin under the European plate. The
three-tectonic regimes in association with the sediments supplies, sea level changes, total basin subsidence, basin
extension, uplifting, and erosion resulted in complex sedimentary packages that are interrupted by many unconformities
and exhibited dramatic lateral facies and thickness changes. Considerable depositional environments
were transited northward, from the reefal and subtidal to shelf and then to the deep marine, where the
facies formation was controlled by mix effects of the sediment supplies, north-tilting continental margin, tectonic
activities, sediment load and subsidence. Offshore part of Sinai preserves good conditions favorable for hydrocarbon
accumulation and requires more intensive exploration.
opening and closure of the Neotethys Ocean. Structural and sedimentological complications related to these
cycles and the basin evolution are selected to be the main targets of the present study in North Sinai. 2D seismic,
boreholes, and outcrop data are used to achieve these targets. The development of the margin began by the
formation of the NE and E-W oriented normal faults during the Jurassic-Early Cretaceous rifting. Two Albian
uplifting phases occurred by the end of this rifting and followed by the Cenomanian-Oligocene positive inversion
that was interrupted by a tectonic loading subsidence phase allowed the deposition of the pelagic Campanian-
Maastrichtian chalk on the shallow Upper Cretaceous carbonate. Shortening related to this inversion inverted
completely the normal-slip on some rift-related faults into reverse faults and related folds or partially inverted by
decreasing of the normal slip on the others. Inversion was ended by the post-Oligocene extensional-subsidence
event that is related to north-sinking of the northern part of the African margin under the European plate. The
three-tectonic regimes in association with the sediments supplies, sea level changes, total basin subsidence, basin
extension, uplifting, and erosion resulted in complex sedimentary packages that are interrupted by many unconformities
and exhibited dramatic lateral facies and thickness changes. Considerable depositional environments
were transited northward, from the reefal and subtidal to shelf and then to the deep marine, where the
facies formation was controlled by mix effects of the sediment supplies, north-tilting continental margin, tectonic
activities, sediment load and subsidence. Offshore part of Sinai preserves good conditions favorable for hydrocarbon
accumulation and requires more intensive exploration.
Other data
Title | Tectonic and basin evolution of South Eastern Mediterranean for hydrocarbon potentiality in North Sinai, Egypt | Authors | Abd-Allah, A.M. ; Ahmed Abd El-Naby; Mohamed H. Abdel Aal | Issue Date | 2020 | Publisher | Elsever | Journal | Journal of Petroleum Science and Engineering | Conference | Inversion tectonics Sinai Eastern Mediterranean basin African continental margin Basin evolution | DOI | 10.1016/j.petrol.2020.107080 |
Recommend this item
Similar Items from Core Recommender Database
Items in Ain Shams Scholar are protected by copyright, with all rights reserved, unless otherwise indicated.