ELEC250 Introduction to Telecommunications by M. Almensori

By M. Almensori

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Des ages de 3 4 0 0 Ma ont été récemment obtenus ( L A T O U C H E , 1 9 7 8 ) dans TEst Hoggar. La signification orogénique de ces ages est douteuse: on ne sait s'il s'agit d'un métamorphisme, d une mise en place de materiel magmatique, de läge du materiel. 2 . - L'orogenése éburnéenne (déf. B O N H O M M E , 1 9 6 2 ) qui separe le Protérozoíque inférieur du Protérozoíque moyen est par contre bien définie. Dans le bouelier ouest-africain on admet 2 0 0 0 ± 1 0 0 Ma comme age avec des episodes tardifs allant jusqu a 1 7 0 0 Ma.

Gr. ( Argilite, breche de silexite, silexite, dolomie de Tifounke. Tifounk* Dolomie, calcaire de Touiderguilt. IStromatolitas IStromatolitM Gris tris fin, siltstone, shale glauconieux, calcaire silteux d'Aouleigate. Calcaire, dolomie, shale d'Aouinet Ould Bou Derballa. IStromatolif. Siltstone, shale glauconieux de l'oued Terrarit. Calcaire, calcaire dolomitique de Tawaz. Gris-quartzite. siltstone, shale calcaire dolomitique de l'oued Tarioufet. ktromatolitM Calcaire, dolomie, shale d'Atar. IStromatolitM Shale, siltstone, dolomie calcaire de Ksar Torchane.

40 Α. - Le socle de lOuest (mole d'Issalane) est formé de métasédiments, de gneiss souvent alcalins et de migmatites. Le contact de ce socle d'áge inconnu et de la Serie de Tiririne, d'áge Protérozoíque supérieur, est toujours anormal: chevauchement vers l'Est évoluant en décrochement dextre. B. - Le socle de l'Est: Formation de Tafassasset-Djanet, encore peu étudiée dans le detail, différe du mole d'Issalane par sa lithologie (abondance de termes volcano-détritiques, enorme développement de granodiorites tardi-tectoniques, datées en U / P b á environ 725 Ma, C A B Y et A N D R E O P O U L O S - R E N A U D , á paraitre) et par son degré de métamorphisme nettement plus faible (faciés de schistes verts pour les termes les plus occidentaux).

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