Please use this identifier to cite or link to this item:
http://dx.doi.org/10.15165/studgeocam-953
Title: | LA STRUTTURA DI M. COSCERNO-RIVODUTRI (APPENNINO UMBRO-MARCHIGIANO): UN SOVRASCORRIMENTO RIUTILIZZATO COME FAGLIA DIRETTA? |
Authors: | TAVARNELLI, E. |
Keywords: | Appennino umbro-marchigiano - Faglie dirette - Sovrascorrimenti - Analisi cinematica Umbria-Marche Apennines - Normal Faults - Thrust Faults - Kinematic Analysis |
Issue Date: | 1995 |
Publisher: | Università di Camerino |
Citation: | Studi geologici camerti, n. speciale, 1995, pp. 611-615 |
Abstract: | The southern part of the Mt. Coscerno-Rivodutri overthrust, located in the southemmost Umbria-Marche Apennines, is described. The overall structure is characterized by a pair of asymmetrical eastward-verging folds whose common overtumed limb is cut by a gently westward-dipping thrust fault. The hangingwall is locally cut by westwarddipping norma! faults whlch terminate against the thrust surface and do not propagate into the footwall. [...] |
URI: | http://193.204.8.201:8080/jspui/handle/1336/320 |
ISSN: | 0392-0631 |
Appears in Volumess: | 1995/1: "Geodinamica e tettonica attiva del sistema Tirreno-Appennino" |
Files in This Item:
File | Description | Size | Format | |
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Vol. Speciale 1995-1 Capitolo 49.pdf | n. speciale, 1995, pp. 611-615 | 533,21 kB | Adobe PDF | View/Open |
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