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A chemical Earth model with whole mantle convection: The importance of a core-mantle boundary layer (D'') and its early formation

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http://pubman.mpdl.mpg.de/cone/persons/resource/persons101004

Hofmann,  A. W.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Tolstikhin, I. N., Kramers, J. D., & Hofmann, A. W. (2006). A chemical Earth model with whole mantle convection: The importance of a core-mantle boundary layer (D'') and its early formation. Chemical Geology, 226(3-4), 79-99.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-8962-1
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