CRUSTAL MOBILITY AND ACTIVE DIAPIRISM SIN CE THE CRETACEOUS PERIOD INTHE TENDE PASS IN THE FRENCH-ITALIAN MARITIME ALPS

Citation
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
Citations number
14
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
12518050
Volume
326
Issue
9
Year of publication
1998
Pages
655 - 662
Database
ISI
SICI code
1251-8050(1998)326:9<655:CMAADS>2.0.ZU;2-H
Abstract
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.