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 | Size | Format | |
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Vol. Speciale 1991-2 Capitolo 54.pdf | n. speciale, 1991, pp. 381-387 | 563,56 kB | Adobe PDF | View/Open |
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