Abstract
Abstract The structure of the Loube massif in Var, France, is typical of the ranges of Provence. The Jurassic cover is divided into a mosaic of independently dislocated segments, reflecting the effects of recurrent movement of basement structures. Development of the mosaic structure and east-west folding in the Cretaceous were succeeded by overthrusting and deformation in the Lutetian-Bartonian (Eocene), with an intervening period of erosion.
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