REPUBLIC OF TUNISIA
Ministry of Industry, Mines and Energy
NOM's RSS Feed
  1.  Rapport d'activités 2023
    Activity Report 2023
  2. Programme Technique 2024
    Technical Program 2024
Outil de recherche métadonnées
  1. REALIZATION OF THE TRAINING PLAN FOR THE YEAR 2022
    REALIZATION OF THE TRAINING PLAN FOR THE YEAR 2022
  2. ACQUISITION OF TWO SERVICE CARS
    ACQUISITION OF TWO SERVICE CARS
  3. ACQUISITION OF GEORADAR EQUIPMENT AND ITS ACCESSORIES
    ACQUISITION OF GEORADAR EQUIPMENT AND ITS ACCESSORIES
Invest in Tunisia
Useful links
Online resources
Online Poll
What do you think of our site ?
Excellent
Very good
Good
Medium


View Poll Results

Search Biblio.
:: Documentation and Editions >> Research library
 

[ Search by author ] [ Search keyword ] [ Search by index ] [ Search by category ]



title of the reference :  Tectonique salifère polyphasée dans la région de Mejez El Bab-Testour (Zone des Domes, Tunisie septentrionale)
Publication Date: 1995
Author : El Ouardi Hmidou, Turki Mohamed Moncef
Catalogue type : Livre
Catalogue reference : 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
Indexation decimale : Tectonique
Keywords : 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
Summary : 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.
Exemplaries : TU1928


 

NOM’s head office 24, Street of Energy, 2035 Charguia - Tunis | BP: 215 - 1080 Tunis Cedex - Tunisia | Phone:(216) 71 808 013 / 71 808 266 - Fax (216) 71 808 098
All rights reserved ©2024 National Office of Mines
Last update :2024-03-28