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title of the reference :
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Tectonique salifère polyphasée dans la région de Mejez El Bab-Testour (Zone des Domes, Tunisie septentrionale)
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Publication Date:
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1995
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Author :
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El Ouardi Hmidou, Turki Mohamed Moncef
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Catalogue type :
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Livre
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Catalogue reference :
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T.XXII, N°2 (FRA) Géol. méditerr. T.XXII, N°2 Tectonique salifère polyphasée dans la région de Mejez El Bab-Testour (Zone des Domes, Tunisie septentrionale) Polyphase salt tectonics in the Mejez El Bab-Testour area (Zone des Domes, northern Tunisia) : control of the meso-cenozoic sedimentation). contrôle de la sédimentation meso-cénozoïque. In Mejez el Bab-Testour area, Triassic domes are the continuity of ech- Chehid dome, they result from polyphased halokinetic motion. The different setting stages can be deduced from the phenomena that occur within the Mesozoic-Cenozoic deposits: reduction in thickness, progressive wedging-out, stratigraphic gaps, intraformational unconformities, hydroplastic deformations and reworking of Triassic material. During the Quaternary and Miocene shortening phases, these dome structures have acquired the current mushroom-shape and have thrusted Barremian to Plio-Quaternary series. bibliogr. Tectonique salifère ; Crétacé ; Cénozoïque ; Processus polyphasé ; Lacune stratigraphique ; déformation ; contrôle tectonique ; biseau ; discordance ; Trias ; Zone des Domes ; Tunisie ; Tunisie Nord Orientale ; Mejez El Bab ; Testour ; J. Bou Rahal ; J. Bou Mous ; J. Mourra ; J. Kechtilou ; J. Chitana ; J. Hendi ; J. Aoud ; J. Jebs Turki Mohamed Moncef El Ouardi Hmidou Tectonique
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Indexation decimale :
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Tectonique
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Keywords :
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Tectonique salifère ; Crétacé ; Cénozoïque ; Processus polyphasé ; Lacune stratigraphique ; déformation ; contrôle tectonique ; biseau ; discordance ; Trias ; Zone des Domes ; Tunisie ; Tunisie Nord Orientale ; Mejez El Bab ; Testour ; J. Bou Rahal ; J. Bou Mous ; J. Mourra ; J. Kechtilou ; J. Chitana ; J. Hendi ; J. Aoud ; J. Jebs
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Summary :
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In Mejez el Bab-Testour area, Triassic domes are the continuity of ech- Chehid dome, they result from polyphased halokinetic motion. The different setting stages can be deduced from the phenomena that occur within the Mesozoic-Cenozoic deposits: reduction in thickness, progressive wedging-out, stratigraphic gaps, intraformational unconformities, hydroplastic deformations and reworking of Triassic material. During the Quaternary and Miocene shortening phases, these dome structures have acquired the current mushroom-shape and have thrusted Barremian to Plio-Quaternary series.
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Exemplaries :
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TU1928
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