The Duration of Magma Ocean Crystallization on the Moon - Evidence from New W Isotope Data for Metals from High-Ti and Low-Ti Mare Basalts

Details The Duration of Magma Ocean Crystallization on the Moon - Evidence from New W Isotope Data for Metals from High-Ti and Low-Ti Mare Basalts The Duration of Magma Ocean Crystallization on the Moon - Evidence from New W Isotope Data for Metals from High-Ti and Low-Ti Mare Basalts

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2385t&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

1

Scientific paper

We obtained new W isotope data for metals from low- and high-Ti mare
basalt. These data are used here to assess the duration of LMO
crystallization and to address the issue why the Hf-W ages of the LMO
(30-50 Myr) is inconsistent with its 146Sm-142Nd age

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