Three‐dimensional instantaneous mantle flow induced by subduction
By C. Piromallo, Thorsten W. Becker, F. Funiciello, C. Faccenna. 2006
187 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/1bc46f5b5786389e7280f6d58b8f99a8ee39d7be
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In Geophysics
- W. Schellart
- Thorsten W. Becker
- C. Faccenna
- F. Funiciello
- M. Long
- S. Lallemand
- A. Heuret
- E. Giuseppe
Citations in the corpus
- Kinematics and flow patterns in deep mantle and upper mantle subduction models: Influence of the mantle depth and slab to mantle viscosity ratio (2008, methodology): “In a numerical equivalent of this experiment, in which rollback-induced mantle flow is investigated with 3D instantaneous flow simulations [ Piromallo et al., 2006, Figure 1b], it is here stated again that no poloidal flow around the slab tip can observed either.”
- Slab stiffness control of trench motion: Insights from numerical models (2008, background): “[63] In general, wide plates stir a larger amount of mantle material than the intermediate ones [ Piromallo et al., 2006, Funiciello et al., 2006].”
- Complex subduction and small-scale convection revealed by body-wave tomography of the western United States upper mantle (2010, background): “Rollback and sinking of the JdF-G slab is thought to drive toroidal flow of oceanic asthenosphere around the slab edge (Zandt and Humphreys, 2008) with an upward poloidal component to direct asthenosphere into the wedge (Piromallo et al., 2006).”
- Mantle dynamics and seismic anisotropy (2010, background): “…the importance of larger-scale 3D flow due to trench migration, both from a laboratory (e.g., Gouillou-Frottier et al., 1995; Kincaid and Griffiths, 2003; Funiciello et al., 2006) and a numerical modeling perspective (e.g., Piromallo et al., 2006; Stegman et al., 2006; Schellart et al., 2007).”
- Trench migration, net rotation and slab-mantle coupling (2008, background): “During its journey from the ridge to the trench the cold temperature of the surface makes the oceanic lithosphere stiffer than the underlyingmantle, allowing its near rigid motion.”