Please use this identifier to cite or link to this item:
http://dx.doi.org/10.15165/studgeocam-1452
Title: | STRUTTURA DEL FRONTE MONTUOSO UMBRO-MARCHIGIANO-SABINO |
Other Titles: | Structure of the Umbria-Marche-Sabina mountain front |
Authors: | DEIANA, G. MAZZOLI, S. PALTRINIERI, W. PIERANTONI, P. P. ROMANO, A. |
Keywords: | Appennino centro-settentrionale - catene a pieghe e sovrascorrimenti - sezioni geologiche - entità dei rigetti dei sovrascorrimenti Central-northern Apennines - fold and thrust belts - geological sections - thrust displacements |
Issue Date: | 2003 |
Publisher: | Università di Camerino |
Citation: | Studi geologici camerti, n. speciale, 2003, pp. 15-36 |
Abstract: | The Umbria-Marche-Sabina mountain front is bounded by a 250 km long, arc-shaped thrust zone extending from Olevano Romano, to the south, to the Foglia River Valley to the north. Along its southern portion ("Olevano-Antrodoco Line" Auct.), this structure produces the tectonic superposition of the UmbriaSabina Meso-Cenozoic succession on top of the Latium-Abruzzi carbonate platform succession. To the north, ("Monti Sibillini Thrust" Auct.) a tectonic repetition of the Umbria-Marche succession occurs along the thrust zone. This consists of two main en-échelon segments. [...] |
URI: | http://193.204.8.201:8080/jspui/handle/1336/829 |
ISSN: | 0392-0631 |
Appears in Volumess: | Volume 2003/1 |
Files in This Item:
File | Size | Format | |
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Vol. 2003-1 Capitolo 2 p.15.pdf Restricted Access | 2,34 MB | Adobe PDF | View/Open Ask to the Librarian |
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