Ag Isotopic Evolution of the Mantle During Accretion: New Constraints from Pd and Ag Metal-Silicate Partitioning
Abstract
Using new metal-silicate partitioning constraints we calculate Ag isotopic composition of the terrestrial and martian mantle.
- Publication:
-
Differentiation: Building the Internal Architecture of Planets
- Pub Date:
- May 2018
- Bibcode:
- 2018LPICo2084.4034R