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- W2019979680 abstract "The finding that magmatic material from the Moon is more enriched in the heavy isotopes of zinc than its terrestrial and Martian analogues prompts fresh thinking about the origin of our natural satellite. See Letter p.376 The heavily favoured theory for the origin of the Earth–Moon system is a giant impact between the proto-Earth and a Mars-sized body. Such a cataclysmic event would have left its mark on the isotopic composition of the Moon, because light isotopes evaporate more readily than heavier ones. Zinc in particular is a powerful indicator of the volatile histories of planets — it undergoes strong isotopic fractionation in planetary rocks, but is hardly fractionated following volcanic activity on Earth. This study compares high-precision zinc isotopic data for lunar basalts, Martian meteorites and terrestrial igneous rocks, and finds that lunar magmatic rocks are enriched in the heavy isotopes of zinc and have lower zinc concentrations than terrestrial or Martian samples. The authors conclude that these variations are the result of large-scale evaporation of zinc in the aftermath of the Moon-forming giant-impact event." @default.
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- W2019979680 date "2012-10-01" @default.
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- W2019979680 title "Galvanized lunacy" @default.
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- W2019979680 doi "https://doi.org/10.1038/490346a" @default.
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