| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9522234 | Earth and Planetary Science Letters | 2005 | 14 Pages |
Abstract
Within uncertainties, samples from Mars (SNC meteorites), HED (eucrites) and the pallasites (average olivine + metal) have the same Fe isotope compositions as the Earth's mantle. This indicates that the solar system is very homogeneous in Fe isotopes. Its average δ56Fe is very close to that of the IRMM-014 standard.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Stefan Weyer, Ariel D. Anbar, Gerhard P. Brey, Carsten Münker, Klaus Mezger, Alan B. Woodland,