Surface wave detectability of transition zone anisotropy induced by non-Newtonian mantle flow - Université de Lille Accéder directement au contenu
Communication Dans Un Congrès Année : 2022

Surface wave detectability of transition zone anisotropy induced by non-Newtonian mantle flow

Fichier non déposé

Dates et versions

hal-03759685 , version 1 (24-08-2022)

Identifiants

  • HAL Id : hal-03759685 , version 1

Citer

John-Keith Magali, Sébastien Merkel, Estelle Ledoux. Surface wave detectability of transition zone anisotropy induced by non-Newtonian mantle flow. EGU General Assembly, May 2022, Vienna, Austria. ⟨hal-03759685⟩
10 Consultations
0 Téléchargements

Partager

Gmail Facebook X LinkedIn More