Abstract
Magmas that have erupted at Earth's surface reveal a potential new mantle source. This source, which is rich in nickel and has a primordial helium isotopic content, may have originated at great depth in the mantle. See Letter p. 393
Cite
CITATION STYLE
APA
Walter, M. J. (2013). Plumbing nickel from the core. Nature, 493(7432), 309–310. https://doi.org/10.1038/nature11852
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