18 citations as recorded by crossref.

1. Archean crustal compositions promote full mantle convection B. Klein et al.
2. Slab stagnation and detachment under northeast China S. Honda
3. Influence of convection regimes of two-layer thermal convection with large viscosity contrast on the thermal and mechanical states at the interface of the two layers: Implications for dynamics in the present-day and past Earth M. Yoshida
4. Long-lived volcanic resurfacing of Venus driven by early collisions S. Marchi et al.
5. Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry T. Barry et al.
6. Thermochemical Mantle Convection with Drifting Deformable Continents: Main Features of Supercontinent Cycle A. Bobrov & A. Baranov
7. Mantle plume heat flux and surface motion periodicities and their implications for the growth of continental crust M. Li et al.
8. The Stability of Dense Oceanic Crust Near the Core‐Mantle Boundary J. Panton et al.
9. Breaking supercontinents; no need to choose between passive or active M. Wolstencroft & J. Davies
10. Numerical studies on the dynamics of two-layer Rayleigh-Bénard convection with an infinite Prandtl number and large viscosity contrasts M. Yoshida & Y. Hamano
11. Mechanisms for the rise of atmospheric oxygen: Bridging surface oxygenation processes and redox conditions of deep interiors Q. Hu et al.
12. Impact of the Rayleigh number and endothermic phase transition on the time behaviour of mantle avalanches M. Herein et al.
13. Strong plates enhance mantle mixing in early Earth R. Agrusta et al.
14. Influence of deep mantle thermal conductivity on the thermochemical evolution of Earth's mantle and core J. Tian et al.
15. A hierarchical mesh refinement technique for global 3-D spherical mantle convection modelling D. Davies et al.
16. A new conceptual model for whole mantle convection and the origin of hotspot plumes M. Yoshida
17. Effect of temperature-dependent viscosity on mantle convection L. Kuslits et al.
18. On the global geodynamic consequences of different phase boundary morphologies G. Morgan et al.