Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 20 June 2003:
Vol. 300. no. 5627, pp. 1939 - 1942
DOI: 10.1126/science.1085844

Reports

A Low-Density M-type Asteroid in the Main Belt

J. L. Margot* and M. E. Brown

The orbital parameters of a satellite revolving around 22 Kalliope indicate that the bulk density of this main-belt asteroid is 2.37 ± 0.4 grams per cubic centimeter. M-type asteroids such as Kalliope are thought to be the disrupted metallic cores of differentiated bodies. The lowdensity indicates that Kalliope cannot be predominantly composed of metal and may be composed of chondritic material with ~30% porosity. The satellite orbit is circular, suggesting that Kalliope and its satellite have different internal structures and tidal dissipation rates. The satellite may be an aggregate of impact ejecta from an earlier collision with Kalliope.

Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.

* To whom correspondence should be addressed. E-mail: margot{at}gps.caltech.edu

Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Oxygen and Asteroids.
T. H. Burbine, A. S. Rivkin, S. K. Noble, T. Mothe-Diniz, W. F. Bottke, T. J. McCoy, M. D. Dyar, and C. A. Thomas (2008)
Reviews in Mineralogy and Geochemistry 68, 273-343
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)