Uranium isotope ratios of Muonionalusta troilite and complications for the absolute age of the IVA iron meteorite core
The crystallization ages of planetary crustal material (given by basaltic meteorites) and planetary cores (given by iron meteorites) provide fiducial marks for the progress of planetary formation, and thus, the absolute ages of these objects fundamentally direct our knowledge and understanding of planet formation and evolution. The lone precise absolute age of planetary core material was previously obtained on troilite inclusions from the IVA iron meteorite Muonionalusta. This previously...[Show more]
|Collections||ANU Research Publications|
|Source:||Earth and Planetary Science Letters|
|01_Brennecka_Uranium_isotope_ratios_of_2018.pdf||1.28 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.