The colfiorito earthquake sequence of september-october 1997: Surface breaks and seismotectonic implications for the central apennines (Italy)

Journal of Earthquake Engineering

Volumn 2, Issue 2, 1998, Pages 291-302

  Basili, R ^a   Bosi, V ^d   Galadini, F ^b   Gallic, R ^d   Meghraoui, M ^b   Messina, P ^b   Moro, M ^c   Sposato, A ^c  

^a SAPIENZA UNIVERSITY OF ROME   (Italy)

^b CNR   (Italy)

^c Servizio Sismico Nazionale ^*  (Italy)

^d Servizio Sismico Nazionale   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0032237646     PISSN: 13632469     EISSN: None     Source Type: Journal    
DOI: 10.1080/13632469809350323     Document Type: Article

References (7)

1. Amato, A. et al. [1997] La sequenza sismica di Colfiorito: sismotettonica e sismogenesi. 16th Gruppo Nazionale di Geofisica della Terra Solida (GNGTS), general assembly, Rome, November 11-13, abstract volume, 119.
2. Calamita, F. and Pizzi, A. [1992] “Tettonica quatemaria nella dorsale appenninica umbro- marchigiana e bacini intrappenninici associati,” Studi Geol. Cam. 92(1), 17-25.
3. Camassi, R. and Stucchi, M. [1997] NT4.1, A parametric catalogue of damaging earthquakes in the Italian area (release NT4.1.1). GNDT, Milano, 66 + XXVII pp. (Internet, http://emidius.itim.mi.cnr.it/NT/home.html)
4. Camassi, R., Galli, P., Molin, D., Monachesi, G. and Morelli, G. [1997] “Rilievo macro- sismico preluninaxe del terremoto umbro-marchigiano di Settembre-Ottobre 1997," Ingegneria sismica 6, (in press).
5. Cello, G., Mazzoli, S., Tondi, E. and Turco, E. [1997] “Active tectonics in the central Apennines and possible implications for seismic hazard analysis in peninsular Italy,” Tectonophysics 272, 43-68.
6. Meghraoui, M. and Camelbeeck, T. [1996] “Fault-fragment: the source of moderatesized earthquakes," European Seismological Commission Abstract volume, pp 47, Reykjavik.
7. Pizzi, A. [1992] “Faglie recenti e origine delle depressioni tettoniche. Esempi dall'Appennino umbro-marchigiano," Ph.D. Thesis, University of Camerino.