Heterogeneous accretion of Earth inferred from Mo-Ru isotope systematics
Abstract
The Mo and Ru isotopic compositions of meteorites and the bulk silicate Earth (BSE) hold important clues about the provenance of Earth's building material. Prior studies have argued that non-carbonaceous (NC) and carbonaceous (CC) meteorite groups together define a Mo-Ru 'cosmic' correlation, and that the BSE plots on the extension of this correlation. These observations were taken as evidence that the final 10-15% of Earth's accreted material...
Paper Details
Title
Heterogeneous accretion of Earth inferred from Mo-Ru isotope systematics
Published Date
Mar 1, 2020
Volume
534
Pages
116065 - 116065
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