Programme annuel & rapport de suivi technique |
-
Programmes Techniques 2025
-
Rapport d'activités 2023
|
Géocatalogue |
|
Appels d'Offres |
-
DESIGNATION D’UN REVISEUR COMPTABLE POUR LES EXERCICES 2025-2026-2027
-
ACQUISITION DE MATERIEL INFORMATIQUE ET EQUIPEMENTS RESEAUX
|
Investir en Tunisie |
|
|
|
::
Documentation and Editions
>>
Research library
|
|
|
[
Search by author
]
[
Search keyword
]
[
Search by index
]
[
Search by category
]
title of the reference :
|
Iron and Copper ore occurences in NW Tunisia.
|
Publication Date:
|
1997
|
Author :
|
El Kashami H., Alouani Rabeh, Tallek S.
|
Catalogue type :
|
Livre
|
Catalogue reference :
|
Iron and Copper ore occurences in NW Tunisia. first Mining Conf in the Great Jamahiriya The study investigated the occurence of iron and copper ores in NW Tunisia. These occurence are withing rock formations belonging to the Triassic and Cretaceous geological ages. Field investigations and petrographical examination indicated a link between these occurences and the tectonic evolution of the region and proved the thermal origin of these veir ores. There are four consequent mineralogical occrences. The occurences of these ores have also some connection with structural, metamorphic development of the region resulting in two sets (NE and NW)of joints and faults. fer ; cuivre ; controle tectonique ; Tunisie ; Tunisie Nord Occidentale Alouani Rabeh Tallek S. El Kashami H. Gîtologie
|
Indexation decimale :
|
Gîtologie
|
Keywords :
|
fer ; cuivre ; controle tectonique ; Tunisie ; Tunisie Nord Occidentale
|
Summary :
|
The study investigated the occurence of iron and copper ores in NW Tunisia. These occurence are withing rock formations belonging to the Triassic and Cretaceous geological ages. Field investigations and petrographical examination indicated a link between these occurences and the tectonic evolution of the region and proved the thermal origin of these veir ores. There are four consequent mineralogical occrences. The occurences of these ores have also some connection with structural, metamorphic development of the region resulting in two sets (NE and NW)of joints and faults.
|
Exemplaries :
|
TU1998
|
|
|
|
|
|