Abstract
The petrologic diversity of meteorites demonstrates that planetesimals ranged from unmelted, variably metamorphosed aggregates to fully molten, differentiated bodies. However, partially differentiated bodies have not been unambiguously identified in the asteroid belt. New constraints on the density, composition, and morphology of 21 Lutetia from the Rosetta spacecraft indicate that the asteroid's high bulk density exceeds that of most known chondritic meteorite groups, yet its surface properties resemble those of some carbonaceous and enstatite chondrite groups. This indicates that Lutetia likely experienced early compaction processes like metamorphic sintering. It may have also partially differentiated, forming a metallic core overlain by a primitive chondritic crust.
Original language | English (US) |
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Pages (from-to) | 137-146 |
Number of pages | 10 |
Journal | Planetary and Space Science |
Volume | 66 |
Issue number | 1 |
DOIs | |
State | Published - Jun 2012 |
Externally published | Yes |
Keywords
- Asteroids
- Chondrites
- Differentiation
- Lutetia
- Metamorphism
- Planetary evolution
- Planetesimals
- Rosetta
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science