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title of the reference :
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Mécanisme d'ouverture des bassins récents liés au système décrochant de Sbiba-Chérichira (Tunisie centrale).
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Publication Date:
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1995
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Author :
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El Ghali Abdessalem, Ben Ayed Noureddine
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Catalogue type :
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Livre
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Catalogue reference :
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T.XXII, N°3-4 (FRA) Géol. méditerr. T.XXII, N°3-4 Mécanisme d'ouverture des bassins récents liés au système décrochant de Sbiba-Chérichira (Tunisie centrale). Opening mechanisms of recent basins linked to the Sbiba-Cherichira (central Tunisia) strike-slip system). In central Tunisia, the lacustrine basins were opened and arranged following a compressional overstep pattern between the E-W strike-slip faults of Sbiba and Cherichira. This pattern has enabled the sedimentation of lacustrine limestone during and after Miocene folding phase. At the beginning of the Pleistocene, several NE-SW folds and NW-SE grabens associated to E-W and N-S strike-slip faults were formed under NW-SE drainage of Marguelli river and enabled installation of Quaternary lacustrine basins. bibliogr. Microtectonique ; Tectonique compression ; Tertiaire ; Pléistocène inf ; Bassin sédimentaire ; Subsidence ; Faille décrochement ; compression ; chavauchement ; Tunisie ; Tunisie Centrale Ben Ayed Noureddine El Ghali Abdessalem Tectonique
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Indexation decimale :
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Tectonique
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Keywords :
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Microtectonique ; Tectonique compression ; Tertiaire ; Pléistocène inf ; Bassin sédimentaire ; Subsidence ; Faille décrochement ; compression ; chavauchement ; Tunisie ; Tunisie Centrale
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Summary :
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In central Tunisia, the lacustrine basins were opened and arranged following a compressional overstep pattern between the E-W strike-slip faults of Sbiba and Cherichira. This pattern has enabled the sedimentation of lacustrine limestone during and after Miocene folding phase. At the beginning of the Pleistocene, several NE-SW folds and NW-SE grabens associated to E-W and N-S strike-slip faults were formed under NW-SE drainage of Marguelli river and enabled installation of Quaternary lacustrine basins.
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Exemplaries :
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TU1945
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