$Inter-mineral Mg isotope fractionation during hydrothermal ultramafic rock alteration: Implications for the global Mg-cycle$
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Inter-mineral Mg isotope fractionation during hydrothermal ultramafic rock alteration: Implications for the global Mg-cycle

Both riverine and ocean waters are enriched in 24Mg compared to the homogeneous chondritic Mg isotopic composition of the Earth's mantle requiring a fractionation step that is generally attributed to low temperature continental crust weathering. Here we present new observations that indicate th...

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Bibliographic Details
Main Authors:	Beinlich, Andreas, Mavromatis, V., Austrheim, H., Oelkers, E.
Format:	Journal Article
Published:	2014
Online Access:	http://hdl.handle.net/20.500.11937/45382

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