Fig. 5

Revised tectonic map of the Voirons Flysch between the Voirons and the Allinges Hills with the location of the type and reference sections. The northern portion beyond the Dranse River is not shown due to the lack of constrains. The geometry along the Allinges Hills is hypothetical in the absence of subsurface data. The Bruant Sandstone is interpreted here as a stratigraphic unit