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Reports
Submitted on December 18, 2007 Ancient Asteroids Enriched in Refractory Inclusions
1 Department of Astronomy, University of Maryland, College Park, MD, 20742, USA. * To whom correspondence should be addressed.
Calcium-, aluminum-rich inclusions (CAIs) occur in all classes of chondritic meteorites and contain refractory minerals predicted to be the first condensates from the solar nebula. Near infrared spectra of CAIs have strong 2 µm absorptions, attributed to FeO-bearing aluminous spinel. Similar absorptions are present in telescopic spectra of several asteroids; modeling indicates these contain ~30±10% CAIs, 2-3 times that of any meteorite. Survival of these undifferentiated, large (50-100 km diameter) CAI-rich bodies argues that they may have formed before the injection of radiogenic 26Al into the Solar System. They have also experienced only modest post-accretionary alteration. Thus, these asteroids have higher concentrations of CAI material, are likely less altered, and are more ancient than any known sample in our meteorite collection, making them prime candidates for sample return.
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