Utilizza questo identificativo per citare o creare un link a questo documento:
http://dx.doi.org/10.15165/studgeocam-1305
Record completo di tutti i metadati
Campo DC | Valore | Lingua |
---|---|---|
dc.contributor.author | BORRACCINI, F. | - |
dc.contributor.author | DE DONATIS, M. | - |
dc.contributor.author | DI BUCCI, D. | - |
dc.contributor.author | MAZZOLI, S. | - |
dc.contributor.author | MEGNA, A. | - |
dc.contributor.author | NESCI, O. | - |
dc.contributor.author | SANTINI, S. | - |
dc.contributor.author | SAVELLI, D. | - |
dc.contributor.author | TRAMONTANA, M. | - |
dc.date.accessioned | 2017-12-04T09:56:03Z | - |
dc.date.available | 2017-12-04T09:56:03Z | - |
dc.date.issued | 2004 | - |
dc.identifier.citation | Studi geologici camerti, n. speciale, 2004, pp. 39-44 | it |
dc.identifier.issn | 0392-0631 | - |
dc.identifier.uri | http://193.204.8.201:8080/jspui/handle/1336/672 | - |
dc.description.abstract | The Quatemary tectonics of the northem Marche sector of the outer Northem Apennines has been analysed. Orogenic structures within the study area include late Miocene - Pliocene, mainly NE verging thrusts and associated folds whose geometry is locally controlled by gliding on oblique and lateral ramp segments. Post-orogenic features consist mainl y of normal and oblique-slip faults resulting from WSW-ENE oriented extension. [...] | en |
dc.publisher | Università di Camerino | it |
dc.subject | Structural geology - Fault reactivation - Geomorphology - Seismotectonics | en |
dc.title | QUATERNARY TECTONICS OF THE NORTHERN MARCHE REGI ON, AND IMPLICATIONS FOR ACTIVE DEFORMATION IN THE OUTER NORTHERN APENNINES | en |
dc.description.pages | 39-44 | - |
E' visualizzato nelle collezioni: | 2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002 |
File in questo documento:
File | Dimensioni | Formato | |
---|---|---|---|
2004 Vol. Speciale Capitolo 8 p.39.pdf | 651,26 kB | Adobe PDF | Visualizza/apri |
Questo documento e' protetto dal copyright originale |
Tutti i documenti archiviati sono protetti da copyright. Tutti i diritti riservati.