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Earth's heterogeneous mantle: A product of convection-driven interaction between crust and mantle

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Stracke,  A.
Geochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Stracke, A. (2012). Earth's heterogeneous mantle: A product of convection-driven interaction between crust and mantle. Chemical Geology, 330, 274-299.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0014-7C7B-3
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