Mechanical coupling of the motion of the surface plate and the lower mantle slab: Effects of viscosity hill, yield strength, and depth-dependent thermal expansivity

Author:

Kaneko Takeo,Nakakuki Tomoeki,Iwamori Hikaru

Funder

Grants-in-Aid for Scientific Research

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference76 articles.

1. Subducting-slab transition-zone interaction: stagnation, penetration and mode switches;Agrusta;Earth Planet. Sci. Lett.,2017

2. A model for the computation of thermal expansivity at high temperatures: MgO as an example;Anderson;Geophys. Res. Lett.,1992

3. The effects of rheological decoupling on slab deformation in the Earth's upper mantle;Androvičová;Stud. Geophys. Geod.,2013

4. Numerical simulations of subduction zones: effects of slab dehydration on the mantle wedge dynamics;Arcay;Phys. Earth Planet. Inter.,2005

5. Arcay, D., Tric, E., Doin, M. P., Bousquet, R., de Capitani, C., 2006. Overriding plate thinning in subduction zones: localized convection induces by slab dehydration. Geochem. Geophys. Geosyst. 7. 1–26. https://doi.org/10.1029/2005GC00106.

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3. Thermal History of the Earth: On the Importance of Surface Processes and the Size of Tectonic Plates;Geochemistry, Geophysics, Geosystems;2020-11

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