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Sequence-stratigraphic interpretation of structurally controlled deposition: Middle Miocene Kareem Formation, southwestern Gulf of Suez, Egypt
Author(s) -
Ahmed Abd El Naby,
Hussam Ghanem,
Mohamed Boukhary,
Mohamed H. Abdel Aal,
Sebastian Lüning,
Jochen Kuss
Publication year - 2010
Publication title -
geoarabia
Language(s) - English
Resource type - Journals
ISSN - 1025-6059
DOI - 10.2113/geoarabia1503129
Subject(s) - facies , geology , palaeogeography , sedimentary depositional environment , paleontology , structural basin , tectonics , sequence (biology) , sedimentary rock , fault block , fault (geology) , deposition (geology) , rift , sequence stratigraphy , block (permutation group theory) , geometry , volcanism , genetics , mathematics , biology
The structural evolution and sequence-stratigraphic architecture of the syn-rift Middle Miocene (Langhian) Kareem Formation were studied in the Western Sub-Basin (WSB) of the Gulf of Suez, Egypt. Biostratigraphic data, facies interpretations, and log data from thirteen wells were used to construct six tectono-sedimentary scenarios and lithofacies-distribution maps, which illustrate the paleogeography during six systems tracts. Abrupt thickness and facies changes reflect deep basins and adjacent high-relief areas created by differential fault-block movements. Within the WSB seven individual fault blocks record complex, tectonically controlled deposition of the Kareem Formation, which we subdivide into two third-order sequences. Earlier tectonic interpretations, facies analysis, and stratigraphic correlations from individual fault blocks were used to interpret the varying depositional settings during six systems tracts and, as a consequence, to discern the structural evolution of the WSB during the Middle Miocene.

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