Articles | Volume 10, issue 3
Solid Earth, 10, 969–985, 2019
https://doi.org/10.5194/se-10-969-2019
Solid Earth, 10, 969–985, 2019
https://doi.org/10.5194/se-10-969-2019

Method article 28 Jun 2019

Method article | 28 Jun 2019

Improving subduction interface implementation in dynamic numerical models

Dan Sandiford and Louis Moresi

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Cited articles

Aagaard, B., Knepley, M., and Williams, C.: PyLith v2.2.1, Computational Infrastructure for Geodynamics, https://doi.org/10.5281/zenodo.886600, 2017. a
Abers, G. A.: Seismic low-velocity layer at the top of subducting slabs: observations, predictions, and systematics, Phys. Earth Planet. Int., 149, 7–29, 2005. a, b
Agrusta, R., Goes, S., and van Hunen, J.: Subducting-slab transition-zone interaction: Stagnation, penetration and mode switches, Earth Planet. Sc. Lett., 464, 10–23, 2017. a, b, c
Alisic, L., Gurnis, M., Stadler, G., Burstedde, C., Wilcox, L. C., and Ghattas, O.: Slab stress and strain rate as constraints on global mantle flow, Geophys. Res. Lett., 37, L22308, https://doi.org/10.1029/2010gl045312, 2010. a, b
Androvičová, A., Čížková, H., and van den Berg, A.: The effects of rheological decoupling on slab deformation in the Earths upper mantle, Stud. Geophys. Geod., 57, 460–481, 2013. a
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This study investigates approaches to implementing plate boundaries within a fluid dynamic framework, targeted at the evolution of subduction over many millions of years.