Tungsten isotopic evidence for disproportional late accretion to the Earth and Moon


Characterization of the hafnium–tungsten systematics (182Hf decaying to 182W and emitting two electrons with a half-life of 8.9 million years) of the lunar mantle will enable better constraints on the timescale and processes involved in the currently accepted giant-impact theory for the formation and evolution of the Moon, and for testing the late-accretion… (More)
DOI: 10.1038/nature14355

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