Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1030
Title: LA STRUTTURA A FALDE DELLA SABINA (APPENNINO CENTRALE)
Authors: COSENTINO, D.
PAROTTO, M.
Keywords: Geologia strutturale - catena a sovrascorrimenti - tettonica pellicolare - dominio sabino - Appennino centrale
Structural geology - Thrust Belt - Thin Skinned Tectonics - Sabine Domain - Central Apennines
Issue Date: 1991
Publisher: Università di Camerino
Citation: Studi geologici camerti, n. speciale, 1991, pp. 381-387
Abstract: The Apenninic Chain is a postcollisional fold and thrust belt originated in an ensialic context by severa! compressive tectonic phases from Paleogene to Pleistocene times. The chain is built up by severa! stratigraphic-structural units overthrust one onto the other with a northeastern orogenic transport. [...]
URI: http://193.204.8.201:8080/jspui/handle/1336/393
ISSN: 0392-0631
Appears in Volumess:1991/2: "Studi preliminari all'acquisizione dati del profilo CROP 11 Civitavecchia-Vasto"

Files in This Item:
File Description SizeFormat 
Vol. Speciale 1991-2 Capitolo 54.pdfn. speciale, 1991, pp. 381-387563,56 kBAdobe PDFView/Open


This item is protected by original copyright



Items in Archive are protected by copyright, with all rights reserved, unless otherwise indicated.