- Lateral variations in CMB heat flux and deep mantle seismic velocity caused by a thermalchemical-phase boundary layer in 3D spherical convection
- Buoyant melting instabilities beneath extending lithosphere: 1. Numerical models
- Large Scale Three-Dimensional Boundary Element Simulation of Subduction
- Earth's core formation aided by flow channelling instabilities induced by iron diapirs Gregor J. Golabek a,b,
- Effects of lowviscosity postperovskite on thermochemical mantle convection in a 3D spherical shell
- Earth Planets Space, 62, 665673, 2010 Construction of semi-dynamic model of subduction zone
- Physics of the Earth and Planetary Interiors 180 (2010) 271282 Contents lists available at ScienceDirect
- Heat partitioning in terrestrial planets during core formation by negative diapirism H. Samuel a,
- Physics of the Earth and Planetary Interiors 178 (2010) 9299 Contents lists available at ScienceDirect
- Numerical modeling of protocore destabilization during planetary accretion: Methodology and results
- Icarus 202 (2009) 429443 Contents lists available at ScienceDirect
- Planforms of self-consistently generated plates in 3D spherical H. J. van Heck1
- Physics of the Earth and Planetary Interiors 171 (2008) 4854 Contents lists available at ScienceDirect
- Mantle Geochemical Geodynamics Chapter for `Treatise on Geophysics' volume edited by D. Bercovici
- than 10 mol% has no further influence on the shape-memory properties. After two cycles of UV irradiation, the clear film turned
- Deep mantle heat flow and thermal evolution of the Earth's core in thermochemical multiphase models of mantle
- Physics of the Earth and Planetary Interiors xxx (2004) xxxxxx Evolution of helium and argon isotopes in a convecting mantle
- Three-Dimensional Spherical Shell Convection at Infinite Prandtl Number Using the `Cubed Sphere' Method
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- submitted to Icarus 2/25/2000 Three-Dimensional Simulations of Mantle Convection in Io
- revised for JGR March 14 2001 Convection in Io's Asthenosphere: Redistribution of Non-uniform
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- TACKLEY ET AL.:THERMO-CHEMICAL PHILOSOPHY Numerical and laboratory studies of mantle convection: Philosophy,
- Testing the tracer ratio method for modeling active compositional fields in mantle convection simulations
- Evolution of U-Pb and Sm-Nd systems in numerical models of mantle convection and plate tectonics
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- coupling of plate tectonics to mantle convection is also a major focus of this project.
- Influence of the Post-Perovskite Transition on Thermal and Thermo-Chemical Mantle Convection
- Physics of the Earth and Planetary Interiors 162 (2007) 149163 Some dynamical consequences of partial melting
- Eects of thermo-chemical mantle convection on the thermal evolution of the Earth's core
- Effects of a perovskite-post perovskite phase change near core-mantle boundary in compressible mantle convection
- Role of ironspin transition in ferropericlase on seismic interpretation: A broad thermochemical transition in the mid
- Volume 11, Number 6 2 June 2010
- Three-dimensional structures and dynamics in the deep mantle: Effects of post-perovskite phase change and deep mantle layering
- Plume heat flow is much lower than CMB heat flow Eric Mittelstaedt a,*, Paul J. Tackley a,b
- The interaction between the post-perovskite phase change and a thermo-chemical boundary layer near the coremantle boundary
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- THREE-DIMENSIONAL SPHERICAL SIMULATIONS OF CONVECTION IN EARTH'S MANTLE AND CORE USING MASSIVELY-PARALLEL COMPUTERS
- Please cite this article in press as: Tackley, P.J., Modelling compressible mantle convection with large viscosity contrasts in a three-dimensional spherical shell using the yin-yang grid. Phys. Earth Planet. Interiors (2008), doi:10.1016/j.pepi.2008.08.0
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- Volume 12, Number 7 8 July 2011
- THREE-DIMENSIONAL SPHERICAL SIMULATIONS OF CONVECTION IN EARTH'S MANTLE AND CORE USING MASSIVELY-PARALLEL COMPUTERS
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- Plate tectonics on super-Earths: Equally or more likely than on Earth H.J. van Heck , P.J. Tackley
- Development of a Stokes flow solver robust to large viscosity jumps using a Schur complement approach with mixed precision arithmetic
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- GEOPHYSICALRF_3EARCHLETTERS,VOL.20,NO.23,PAGES2599-2602,DECEMBER14,1993 ON THE PENETRATION OF THE 660 KM PHASE CHANGE BY MANTLE DOWNFLOWS
- PUBLISHED ONLINE: 26 JUNE 2011 | DOI: 10.1038/NGEO1187 Spatial and temporal variability in Hawaiian
- A free plate surface and weak oceanic crust produce single-sided subduction on Earth
- Dynamics and evolution of the deep mantle resulting from thermal, chemical, phase and melting effects
