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Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle

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Chen,  M.
Cosmochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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El Goresy,  A.
Cosmochemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Chen, M., El Goresy, A., Frost, D., & Gillet, P. (2004). Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle. European Journal of Mineralogy, 16(2), 203-211.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0014-8CF2-1
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