A benchmark study on mantle convection in a 3-D spherical shell using CitcomS

Author:

Zhong Shijie1,McNamara Allen2,Tan Eh3,Moresi Louis4,Gurnis Michael5

Affiliation:

1. Department of Physics; University of Colorado; Boulder; Colorado; 80309; USA

2. School of Earth and Space Exploration; Arizona State University; Tempe; Arizona; 85287; USA

3. Computational Infrastructure for Geodynamics; California Institute of Technology; Pasadena; California; 91125; USA

4. School of Mathematical Sciences; Monash University; Clayton; Victoria 3800; Australia

5. Seismological Laboratory; California Institute of Technology; Pasadena; California; 91125; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference69 articles.

1. Iterative methods for stabilized mixed velocity-pressure finite elements;Atanga;Int. J. Numer. Methods Fluids,1992

2. Three-dimensional treatment of convective flow in the Earth's mantle;Baumgardner;J. Stat. Phys.,1985

3. On the effect of temperature and strain-rate dependent viscosity on global mantle flow, net rotation, and plate-driving forces;Becker;Geophys. J. Int.,2006

4. Azimuthal seismic anisotropy constrains net rotation of the lithosphere;Becker;Geophys. Res. Lett.,2008

5. The generation of plate tectonics from mantle convection;Bercovici;Earth Planet. Sci. Lett.,2003

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