NEOGENE EVOLUTION OF AN ARCUATE STRUCTURE IN THE UMBRIA-MARCHE APENNINES
The Umbria-Marche Apennines is an arcuate fold and thrust belt, built up during Upper Miocene-Pliocene. Folds and thrusts affect at the surface the sedimentary cover. The AA. examine the innermost ridge in the sector between M. Nerone to the north and M. Serano to the south. lt is made up of a dext...
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Milano University Press
2017-08-01
|
| Series: | Rivista Italiana di Paleontologia e Stratigrafia |
| Subjects: | |
| Online Access: | https://riviste.unimi.it/index.php/RIPS/article/view/9040 |