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Volume 8, issue 5
Solid Earth, 8, 899–919, 2017
https://doi.org/10.5194/se-8-899-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Solid Earth, 8, 899–919, 2017
https://doi.org/10.5194/se-8-899-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Sep 2017

Research article | 11 Sep 2017

Global patterns in Earth's dynamic topography since the Jurassic: the role of subducted slabs

Michael Rubey et al.
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Cited articles  
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Boyden, J. A., Müller, R. D., Gurnis, M., Torsvik, T. H., Clark, J. A., Turner, M., Ivey-Law, H., Watson, R. J., and Cannon, J. S.: Next-generation plate-tectonic reconstructions using GPlates, in Geoinformatics, Cambridge University Press, 95–114, https://doi.org/10.1017/CBO9780511976308.008, 2011.
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Bunge, H.-P., Richards, M. A., and Baumgardner, J. R.: A sensitivity study of three-dimensional spherical mantle convection at 108 Rayleigh number: Effects of depth-dependent viscosity, heating mode, and an endothermic phase change, J. Geophys. Res.-Sol. Ea., 102, 11991–12007, https://doi.org/10.1029/96JB03806, 1997.
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Short summary
Earth's surface is constantly warped up and down by the convecting mantle. Here we derive geodynamic rules for this so-called dynamic topography by employing high-resolution numerical models of global mantle convection. We define four types of dynamic topography history that are primarily controlled by the ever-changing pattern of Earth's subduction zones. Our models provide a predictive quantitative framework linking mantle convection with plate tectonics and sedimentary basin evolution.
Earth's surface is constantly warped up and down by the convecting mantle. Here we derive...
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