The E-W trending Souli Fault exhibits geological evidence of past individual coseismic events. Along some sectors of the fault, young morphotectonic features have been recognized thereby emphasising the recent tectonic activity. At least three distinct events pre- and post-dating wedge layers of 20 ka to 26 ka lignite-type sediments have been recognised.

Palaeoseismicity of the Souli Fault, Epirus, Western Greece

CAPUTO, Riccardo;
1997

Abstract

The E-W trending Souli Fault exhibits geological evidence of past individual coseismic events. Along some sectors of the fault, young morphotectonic features have been recognized thereby emphasising the recent tectonic activity. At least three distinct events pre- and post-dating wedge layers of 20 ka to 26 ka lignite-type sediments have been recognised.
1997
Boccaletti, M.; Caputo, Riccardo; Mountrakis, D.; Pavlides, S.; Zouros, N.
File in questo prodotto:
Non ci sono file associati a questo prodotto.

I documenti in SFERA sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/460963
 Attenzione

Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo

Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 16
  • ???jsp.display-item.citation.isi??? ND
social impact