Determination of the Bulk Silicate Moon FeO Content from Petrological and Geophysical Models
Abstract
We determined the bulk silicate Moon FeO content by combining models of magma ocean solidification and mantle convection with observational constraints on the stratigraphy, bulk Moon density, and moment of inertia from seismic and selenodetic data.
- Publication:
-
52nd Lunar and Planetary Science Conference
- Pub Date:
- March 2021
- Bibcode:
- 2021LPI....52.2089S