• DOI:10.1038/nature04751
• Corpus ID: 4373614

Discovery of a 25-cm asteroid clast in the giant Morokweng impact crater, South Africa

@article{Maier2006DiscoveryOA,
  title={Discovery of a 25-cm asteroid clast in the giant Morokweng impact crater, South Africa},
  author={Wolfgang D. Maier and Marco A. G. Andreoli and Iain McDonald and Michael Denis Higgins and Adrian J Boyce and Alexander Shukolyukov and Gunter W. Lugmair and Lewis D. Ashwal and Peter P. H. Gr{\"a}ser and Edward M. Ripley and Rodger J. Hart},
  journal={Nature},
  year={2006},
  volume={441},
  pages={203-206}
}

• W. Maier, M. Andreoli, +8 authors R. J. Hart
• Published 1 May 2006
• Geology
• Nature

Meteorites provide a sample of Solar System bodies and so constrain the types of objects that have collided with Earth over time. Meteorites analysed to date, however, are unlikely to be representative of the entire population and it is also possible that changes in their nature have occurred with time. Large objects are widely believed to be completely melted or vaporized during high-angle impact with the Earth. Consequently, identification of large impactors relies on indirect chemical tracers, notably the platinum-group elements. Here we report the discovery of a large (25-cm), unaltered, fossil meteorite, and several smaller fragments within the impact melt of the giant (> 70 km diameter), 145-Myr-old Morokweng crater, South Africa. The large fragment (clast) resembles an LL6 chondrite breccia, but contains anomalously iron-rich silicates, Fe-Ni sulphides, and no troilite or metal. It has chondritic chromium isotope ratios and identical platinum-group element ratios to the bulk impact melt. These features allow the unambiguous characterization of an impactor at a large crater. Furthermore, the unusual composition of the meteorite suggests that the Morokweng asteroid incorporated part of the LL chondrite parent body not represented by objects at present reaching the Earth.