Les phases tectoniques du NE du Devoluy et leur influence structurologique

Abstract
A detailed study of the structure of the northeastern part of the Devoluy region, France, shows that the superimposed effects of different tectonic phases (Turonian and Alpine) can be recognized on the scale of the fold and of the microfold. Geodynamic solutions are proposed for analysis of the effects of erosion, differential behavior of limestones and plastic beds, landslides, and isostatic readjustment which intervened during deformation.

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