15 citations as recorded by crossref.

1. Can subduction initiation at a transform fault be spontaneous? D. Arcay et al. 10.5194/se-11-37-2020
2. Linked influences on slab stagnation: Interplay between lower mantle viscosity structure, phase transitions, and plate coupling H. Čížková & C. Bina 10.1016/j.epsl.2018.12.027
3. Tectonic Stacking of HP/LT Metamorphic Rocks in Accretionary Wedges and the Role of Shallowing Slab‐Mantle Decoupling M. Aygül & R. Oberhänsli 10.1002/2017TC004689
4. Sea-level stability over geological time owing to limited deep subduction of hydrated mantle N. Cerpa et al. 10.1038/s41561-022-00924-3
5. Improving subduction interface implementation in dynamic numerical models D. Sandiford & L. Moresi 10.5194/se-10-969-2019
6. The influence of viscous slab rheology on numerical models of subduction N. Hummel et al. 10.5194/se-15-567-2024
7. Mantle wedge temperatures and their potential relation to volcanic arc location A. Perrin et al. 10.1016/j.epsl.2018.08.011
8. Melt Focusing Along Permeability Barriers at Subduction Zones and the Location of Volcanic Arcs G. Ha et al. 10.1029/2020GC009253
9. Timescales of successful and failed subduction: insights from numerical modelling B. Knight et al. 10.1093/gji/ggaa410
10. Reconciling mantle wedge thermal structure with arc lava thermobarometric determinations in oceanic subduction zones A. Perrin et al. 10.1002/2016GC006527
11. Modelling the interplate domain in thermo-mechanical simulations of subduction: Critical effects of resolution and rheology, and consequences on wet mantle melting D. Arcay 10.1016/j.pepi.2017.05.008
12. Slab Temperature Evolution Over the Lifetime of a Subduction Zone A. Holt & C. Condit 10.1029/2020GC009476
13. Forearc structure in the Lesser Antilles inferred from depth to the Curie temperature and thermo-mechanical simulations L. Gailler et al. 10.1016/j.tecto.2017.03.014
14. Slab to back-arc to arc: Fluid and melt pathways through the mantle wedge beneath the Lesser Antilles S. Hicks et al. 10.1126/sciadv.add2143
15. Subduction zone intermediate-depth seismicity: Insights from the structural analysis of Alpine high-pressure ophiolite-hosted pseudotachylyte (Corsica, France) R. Magott et al. 10.1016/j.jsg.2016.04.002