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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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