According to Héritier and Villemin 38 , it is unlikely to be a continuous fault, but rather a network of relayed segmented faults, along a meridian direction, with a slight trend towards the north-west north of Rambouillet.
← all excerpts
A 3D geomodel of the deep aquifers in the Orléans area of the southern Paris Basin (France).
1
—
—