Hf-W Chronometry of the Moon - New Results from Ferroan Anorthosites and Low-Ti Mare Basalt 15555

Physics

Scientific paper

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Scientific paper

New Hf-W data for ferroan anorthosites show that the lunar crust and
mantle have identical 182W/184W, indicating crust
formation >60 Ma after CAI formation. We show that, in contrast to
earlier reports, low-Ti mare basalt 15555 has no 182W
anomaly.

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