Model data repository of "How sediment thickness influences subduction dynamics and seismicity"
Silvia Brizzi +4 more
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The asthenosphere is commonly defined as an upper mantle zone with low velocities and high attenuation of seismic waves, and high electrical conductivity. These observations are usually explained by the presence of partial melt, or by a sharp contrast in
V. Patočka, H. Čížková, J. Pokorný
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Seismic velocity azimuthal anisotropy of the Japan subduction zone: Constraints from P and S wave traveltimes [PDF]
Xin Liu, Dapeng Zhao
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Plume‐Driven Subduction Termination in 3‐D Mantle Convection Models
The effect of mantle plumes is secondary to that of subducting slabs for modern plate tectonics when considering plate driving forces. However, the impact of plumes on tectonics and planetary surface evolution may nonetheless have been significant.
Erin Heilman, Thorsten W. Becker
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Crustal earthquake triggering by modern great earthquakes on subduction zone thrusts [PDF]
Joan Gomberg, Brian L. Sherrod
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Reconstruction of meratus by subduction modelling around Java, Borneo and Celebes Islands
Joko Soesilo +5 more
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Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific [PDF]
Rupert Sutherland +12 more
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High‐resolution subduction zone seismicity and velocity structure beneath Ibaraki Prefecture, Japan [PDF]
D. R. Shelly +4 more
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Mantle Flow and Anisotropy in Subduction Zones: Modeling and Clustering of Olivine Textures
The mantle near Earth's subduction zones endures intense deformation that generates anisotropic rock textures. These textures can be observed seismically and modeled geodynamically, but the complexity of this deformation makes analyses of these textures ...
Yijun Wang +3 more
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