Fig. 3From: Mimicking Alpine thrusts by passive deformation of synsedimentary normal faults: a record of the Jurassic extension of the European margin (Mont Fort nappe, Pennine Alps)Late Jurassic transect of the Briançonnais s.l. paleogeographic domain in SW Switzerland (after i.a. Trümpy 1960; Baud and Septfontaine 1980; Sartori 1990; Septfontaine 1995; Plancherel et al. 1998; Mohn et al. 2010, 2012; Decarlis et al. 2017a). The distance between the Préalpes Médianes Rigides and the Breccia nappe basins is uncertain and represents a minimal estimate (the domain separating these 2 basins is often referred to as Ultrabriançonnais)Back to article page