Low plume excess temperature and high core heat flux inferred from non-adiabatic geotherms in internally heated mantle circulation models-Reference-Cited by-同舟云学术

Low plume excess temperature and high core heat flux inferred from non-adiabatic geotherms in internally heated mantle circulation models

Published:2005-11 Issue:1-3 Volume:153 Page:3-10
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Bunge Hans-Peter

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference38 articles.

1. High- and low-resolution images of the Earth’s mantle: Implications of different approaches to tomographic modeling;Boschi;J. Geophys. Res.,1999

2. Effect of depth-dependent viscosity on the planform of mantle convection;Bunge;Nature,1996

3. A sensitivity study of three-dimensional spherical mantle convection at 10 (8) Rayleigh number. Effects of depth-dependent viscosity, heating mode, and an endothermic phase change;Bunge;J. Geophys. Res.,1997

4. Time scales and heterogeneous structure in geodynamic earth models;Bunge;Science,1998

5. Non-adiabaticity in mantle convection;Bunge;Geophys. Res. Lett.,2001

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