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Contrasting bulk and mineral chemistry in depleted mantle peridotites: evidence for reactive porous flow

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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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Rampone, E., Romairone, A., & Hofmann, A. W. (2004). Contrasting bulk and mineral chemistry in depleted mantle peridotites: evidence for reactive porous flow. Earth and Planetary Science Letters, 218(3-4), 491-506.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-8D06-D
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