Jp. Ivaldi et al., CRUSTAL MOBILITY AND ACTIVE DIAPIRISM SIN CE THE CRETACEOUS PERIOD INTHE TENDE PASS IN THE FRENCH-ITALIAN MARITIME ALPS, Comptes rendus de l'Academie des sciences. Serie 2. Sciences de la terre et des planetes, 326(9), 1998, pp. 655-662
Sedimentary, tectonic, morphotectonic and rock mechanic data all show
that the Tende pass site in the French-Italian Maritime Alps is a crus
tal block which has been particularly mobile since at least the Upper
Triassic era. This mobility has led to the development of an early dia
pirism, which is still active. (C) Academie des sciences/Elsevier, Par
is.