Iron isotopes may reveal the redox conditions of mantle melting from Archean to Present
High-precision Fe isotopic data for 104 samples, including modern and ancient (≥ 3.7 Ga) subduction-related magmas and mantle peridotites, are presented. These data demonstrate that mid-ocean ridge and oceanic-island basalts (MORBs and OIBs) have on ave
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|Source:||Earth and Planetary Science Letters|
|01_Dauphas_Iron_isotopes_may_reveal_the_2009.pdf||1.05 MB||Adobe PDF||Request a copy|
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