Articles | Volume 2, issue 2
https://doi.org/10.5194/se-2-315-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-2-315-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
19 Dec 2011
Research article |
| 19 Dec 2011
Influence of the Ringwoodite-Perovskite transition on mantle convection in spherical geometry as a function of Clapeyron slope and Rayleigh number
M. Wolstencroft
now at: University of Ottawa, Ottawa, Ontario, Canada
School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff, Wales, CF10 3AT, UK
J. H. Davies
School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff, Wales, CF10 3AT, UK
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Cited
18 citations as recorded by crossref.
- Archean crustal compositions promote full mantle convection B. Klein et al. 10.1016/j.epsl.2017.07.003
- Slab stagnation and detachment under northeast China S. Honda 10.1016/j.tecto.2016.01.025
- 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 10.1063/1.5119753
- Long-lived volcanic resurfacing of Venus driven by early collisions S. Marchi et al. 10.1038/s41550-023-02037-2
- Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry T. Barry et al. 10.1038/s41598-017-01816-y
- Thermochemical Mantle Convection with Drifting Deformable Continents: Main Features of Supercontinent Cycle A. Bobrov & A. Baranov 10.1007/s00024-019-02164-w
- Mantle plume heat flux and surface motion periodicities and their implications for the growth of continental crust M. Li et al. 10.1016/j.epsl.2023.118148
- The Stability of Dense Oceanic Crust Near the Core‐Mantle Boundary J. Panton et al. 10.1029/2022JB025610
- Breaking supercontinents; no need to choose between passive or active M. Wolstencroft & J. Davies 10.5194/se-8-817-2017
- Numerical studies on the dynamics of two-layer Rayleigh-Bénard convection with an infinite Prandtl number and large viscosity contrasts M. Yoshida & Y. Hamano 10.1063/1.4966685
- Mechanisms for the rise of atmospheric oxygen: Bridging surface oxygenation processes and redox conditions of deep interiors Q. Hu et al. 10.1360/TB-2023-0109
- Impact of the Rayleigh number and endothermic phase transition on the time behaviour of mantle avalanches M. Herein et al. 10.1016/j.jog.2013.02.007
- Strong plates enhance mantle mixing in early Earth R. Agrusta et al. 10.1038/s41467-018-05194-5
- A hierarchical mesh refinement technique for global 3-D spherical mantle convection modelling D. Davies et al. 10.5194/gmd-6-1095-2013
- A new conceptual model for whole mantle convection and the origin of hotspot plumes M. Yoshida 10.1016/j.jog.2014.04.004
- Effect of temperature-dependent viscosity on mantle convection L. Kuslits et al. 10.1007/s40328-014-0055-7
- Conditions of appearance of the asthenospheric layer under upper mantle convection Y. Perepechko & V. Sharapov 10.1134/S1028334X14070241
- The stability and structure of primordial reservoirs in the lower mantle: insights from models of thermochemical convection in three-dimensional spherical geometry Y. Li et al. 10.1093/gji/ggu295
16 citations as recorded by crossref.
- Archean crustal compositions promote full mantle convection B. Klein et al. 10.1016/j.epsl.2017.07.003
- Slab stagnation and detachment under northeast China S. Honda 10.1016/j.tecto.2016.01.025
- 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 10.1063/1.5119753
- Long-lived volcanic resurfacing of Venus driven by early collisions S. Marchi et al. 10.1038/s41550-023-02037-2
- Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry T. Barry et al. 10.1038/s41598-017-01816-y
- Thermochemical Mantle Convection with Drifting Deformable Continents: Main Features of Supercontinent Cycle A. Bobrov & A. Baranov 10.1007/s00024-019-02164-w
- Mantle plume heat flux and surface motion periodicities and their implications for the growth of continental crust M. Li et al. 10.1016/j.epsl.2023.118148
- The Stability of Dense Oceanic Crust Near the Core‐Mantle Boundary J. Panton et al. 10.1029/2022JB025610
- Breaking supercontinents; no need to choose between passive or active M. Wolstencroft & J. Davies 10.5194/se-8-817-2017
- Numerical studies on the dynamics of two-layer Rayleigh-Bénard convection with an infinite Prandtl number and large viscosity contrasts M. Yoshida & Y. Hamano 10.1063/1.4966685
- Mechanisms for the rise of atmospheric oxygen: Bridging surface oxygenation processes and redox conditions of deep interiors Q. Hu et al. 10.1360/TB-2023-0109
- Impact of the Rayleigh number and endothermic phase transition on the time behaviour of mantle avalanches M. Herein et al. 10.1016/j.jog.2013.02.007
- Strong plates enhance mantle mixing in early Earth R. Agrusta et al. 10.1038/s41467-018-05194-5
- A hierarchical mesh refinement technique for global 3-D spherical mantle convection modelling D. Davies et al. 10.5194/gmd-6-1095-2013
- A new conceptual model for whole mantle convection and the origin of hotspot plumes M. Yoshida 10.1016/j.jog.2014.04.004
- Effect of temperature-dependent viscosity on mantle convection L. Kuslits et al. 10.1007/s40328-014-0055-7
2 citations as recorded by crossref.
- Conditions of appearance of the asthenospheric layer under upper mantle convection Y. Perepechko & V. Sharapov 10.1134/S1028334X14070241
- The stability and structure of primordial reservoirs in the lower mantle: insights from models of thermochemical convection in three-dimensional spherical geometry Y. Li et al. 10.1093/gji/ggu295
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