The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional structure located at the transition between ongoing contractional and extensional crustal compartments above the western edge of the downgoing Ionian slab. Onshore structural data, an offshore seismic reflection profile, and earthquake data are here analyzed to constrain the present geometry of the Tindary Fault System and its tectonic evolution since Neogene, with particular regard to the present and recent activity.
BILLI A, BARBERI G, FACCENNA C, NERI G, PEPE F, SULLI A (2006). Sismotettonica della Faglia di Tindari e delle aree adiacenti (Sicilia nord-orientale). In Riunione Annuale Scientifica del Gruppo Italiano di Geologia Strutturale - Riassunti e note brevi (pp.81-81). ROMA : Società Geologica Italiana.
Sismotettonica della Faglia di Tindari e delle aree adiacenti (Sicilia nord-orientale)
PEPE, Fabrizio;SULLI, Attilio
2006-01-01
Abstract
The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional structure located at the transition between ongoing contractional and extensional crustal compartments above the western edge of the downgoing Ionian slab. Onshore structural data, an offshore seismic reflection profile, and earthquake data are here analyzed to constrain the present geometry of the Tindary Fault System and its tectonic evolution since Neogene, with particular regard to the present and recent activity.
| File | Dimensione | Formato | |
|---|---|---|---|
|
Billi.pdf
Solo gestori archvio
Dimensione
923.04 kB
Formato
Adobe PDF
|
923.04 kB | Adobe PDF | Visualizza/Apri Richiedi una copia |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
