A global geochemical model for the evolution of the mantle
Author:
Publisher
American Geophysical Union
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/GD005p0006/fullpdf
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2. Boundary-layer model of mantle plumes with thermal and chemical diffusion and buoyancy;Geophysical Journal International;2007-04-02
3. Hotspot distribution, gravity, mantle tomography: evidence for plumes;Journal of Geodynamics;1999-03
4. The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.;Terra Nova;1998-07
5. Computation of seismic profiles from mineral physics: the importance of the non-olivine components for explaining the 660 km depth discontinuity;Physics of the Earth and Planetary Interiors;1998-04
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