Geodynamo reversal frequency and heterogeneous core–mantle boundary heat flow-Reference-Cited by-同舟云学术

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Geodynamo reversal frequency and heterogeneous core–mantle boundary heat flow

Published:2010-05 Issue:1-2 Volume:180 Page:66-79
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:

Olson Peter L.,Coe Robert S.,Driscoll Peter E.,Glatzmaier Gary A.,Roberts Paul H.

Publisher

Elsevier BV

Subject

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

Reference87 articles.

1. Constraints on the composition of the Earth’s core from ab initio calculations;Alfe;Nature,2000

2. A simple model for mantle-driven flow at the top of Earth’s core;Amit;Earth Planets Space,2008

3. The magnetic structure of convection-driven numerical dynamos;Aubert;Geophys. J. Int.,2008

4. Thermo-chemical wind flows couple Earth’s inner core growth to mantle heterogeneity;Aubert;Nature,2008

5. Equations governing convection in Earth’s core and the geodynamo;Braginsky;Geophys. Astrophys. Fluid Dyn.,1995

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