The Oligo-Miocene siliciclastic foreland basin deposits of northern Tunisia:Stratigraphy, sedimentology and paleogeography

被引:14
|
作者
Boukhalfa, Kamel [1 ,2 ]
Soussi, Mohamed [2 ]
Ozcan, Ercan [3 ]
Banerjee, Santanu [4 ]
Tounekti, Abdelbasset [2 ]
机构
[1] Univ Carthage, Fac Sci Bizerte, Jarzouna 7021, Tunisia
[2] Univ Tunis El Manar, Fac Sci Tunis, LR18ES07, Tunis 2092, Tunisia
[3] Istanbul Tech Univ, Fac Mines, TR-34469 Istanbul, Turkey
[4] Indian Inst Technol, Mumbai 400076, Maharashtra, India
关键词
Stratigraphy; Sedimentology; Paleogeography; Flexural sub-basin; Oligo-miocene; Northern Tunisia; Peri-tethys; HUMMOCKY CROSS-STRATIFICATION; SEA-LEVEL RISE; SEQUENCE STRATIGRAPHY; NEOGENE DEFORMATION; NUMIDIAN FORMATION; PETROLEUM GEOLOGY; FACIES ANALYSIS; MESAVERDE GROUP; TELLIAN DOMAIN; WESTERN KUTCH;
D O I
10.1016/j.jafrearsci.2020.103932
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper presents an integrated study aiming to assess the stratigraphy, sedimentology and paleogeography of the marine and non-marine Tellian, Bejaoua and Fortuna Oligo-Miocene deposits of northern Tunisia. The fossiliferous strata, particularly the glauconite-rich facies, bounded by major unconformities, refine the stratigraphic framework and address the spatio-temporal relationship between marine and non-marine deposits. Three new updated paleogeographic maps for the Oligocene (30-27 Ma) and the Miocene (21-20 Ma and 15 Ma) epochs, outlining the major transgressive and regressive events and the relationships between the Tellian and Atlasic basins have been produced. The genesis and evolution of the Oligo-Miocene foreland sub-basins of the Tellian, the salt domes zone and the northern Atlas are reconstructed considering the geodynamic events that accompanied the African-Eurasian convergence, besides eustasy and climate.
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页数:20
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