Les terrains allochtones de la napp

Les terrains allochtones de la nappe prérifaine se sont mis en place au Tortonien. Ils sont constitués de Trias argileux et gypsifère qui recouvre le Miocène. Le Trias présente également des dolomies, du gypse et des ophites. Le Lias est représenté par des calcaires et dolomies au-dessus desquels reposent des marno- calcaires du Toarcien-Aalénien. Le Crétacé est essentiellement schisto-gréseux et devient marneux par endroits.

Résultats (Anglais) 1:

Allochthonous prerifaine water courses are set up in the Tortonian. They consist of Triassic clayey and gypsifere overlying the Miocene. This Triassic also dolomite, gypsum and the ophites. The Lias is represented by limestones and dolostones above which are based of marl-limestone of the Toarcian-Aalenian. The Cretaceous is essentially schisto-sandstone and marl in places.

Résultats (Anglais) 2:

Non-native land of prérifaine table were set up in the Tortonian. They are made of clay and gypsiferous Trias overlying Miocene. Trias also presents dolomite, gypsum and ophites. The Lias is represented by limestones and dolomites above which rely limestone marno- Toarcian-Aalenian. The Cretaceous is mainly shale and sandstone and marl becomes places.

Résultats (Anglais) 3:

The allochthonous land pad prerifaine se are put in place at Tortonien. They are composed of Triassic clayey and gypsifere that covers the early Miocene. The Trias also presents the Dolomites, gypsum and the ophites. The Media Economics is represented by of limestones and dolomites above which are based of lime marls- lime of Toarcien-Aalenien .The Cretaceous is essentially at Skhistos-sandstone and becomes has very low climatic demands by places.