Low friction along the high slip patch of the 2011 Mw 9.0 Tohoku-Oki earthquake required from the wedge structure and extensional splay faults - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Geophysical Research Letters Année : 2013

Low friction along the high slip patch of the 2011 Mw 9.0 Tohoku-Oki earthquake required from the wedge structure and extensional splay faults

Résumé

We analyze the mechanical properties needed to account for the large shallow slip during the 2011 Tohoku-Oki earthquake and the activation of landward normal faulting within the forearc. We show that the morphology and internal structure of the forearc follows closely the prediction of the critical Coulomb wedge in horizontal compression, implying a high internal pore pressure ratio ( = 0.7 + 0.14/ – 0.48) and a low effective basal friction (eff b = 0.14 + 0.18/ – 0.04). We then show that the activation of the normal fault requires a lower effective basal friction beneath the outer wedge than beneath the inner wedge (outer 0.015), possibly due to transient dynamic weakening associated to the seismic rupture. Forearc normal faults could be considered as evidence for very efficient dynamic weakening along the megathrust and typify megathrust with high tsunamigenic potential.

Domaines

Tectonique
Fichier principal
Vignette du fichier
Cubas_etal_GRL13.pdf (584.91 Ko) Télécharger le fichier
Origine : Fichiers produits par l'(les) auteur(s)
Loading...

Dates et versions

hal-01482578 , version 1 (03-03-2017)

Identifiants

Citer

Nadaya Cubas, Jean-Philippe Avouac, Yves M. Leroy, Adeline P Pons. Low friction along the high slip patch of the 2011 Mw 9.0 Tohoku-Oki earthquake required from the wedge structure and extensional splay faults. Geophysical Research Letters, 2013, 40, pp.4231 - 4237. ⟨10.1002/grl.50682⟩. ⟨hal-01482578⟩
163 Consultations
92 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More