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Published in 2019 at "Nature Geoscience"
DOI: 10.1038/s41561-019-0446-z
Abstract: Partial melting of Earth’s mantle generates oceanic crust and leaves behind a chemically depleted residual mantle. The time-integrated composition of this chemically depleted mantle is generally inferred from basalts produced at mid-ocean ridges. However, isotopic…
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Keywords:
ultra depleted;
mid ocean;
mantle plume;
depleted mantle ... See more keywords