Lithospheric-scale analogue models are used to analyse the parameters controlling the typical evolution of deformation during continental narrow rifting, characterized by early activation of large boundary faults and basin subsidence, followed by localization of tectonic activity in internal faults at the rift axis.
Inward migration of faulting during continental rifting: Effects of pre-existing lithospheric structure and extension rate / G Corti; G Ranalli; A Agostini; D Sokoutis. - In: TECTONOPHYSICS. - ISSN 0040-1951. - ELETTRONICO. - 594:(2013), pp. 137-148. [10.1016/j.bbr.2011.03.031]
Inward migration of faulting during continental rifting: Effects of pre-existing lithospheric structure and extension rate
CORTI, GIACOMO;AGOSTINI, ANDREA;
2013
Abstract
Lithospheric-scale analogue models are used to analyse the parameters controlling the typical evolution of deformation during continental narrow rifting, characterized by early activation of large boundary faults and basin subsidence, followed by localization of tectonic activity in internal faults at the rift axis.
File in questo prodotto:
| File | Dimensione | Formato | |
|---|---|---|---|
|
Inward migration of faulting during continental rifting.pdf
Accesso chiuso
Tipologia:
Versione finale referata (Postprint, Accepted manuscript)
Licenza:
Open Access
Dimensione
1.32 MB
Formato
Adobe PDF
|
1.32 MB | Adobe PDF | Richiedi una copia |
I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
