Color and Albedo Heterogeneity of Vesta from Dawn

  • Vishnu Reddy
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Andreas Nathues
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Lucille Le Corre
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Holger Sierks
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Jian-Yang Li
    Department of Astronomy, University of Maryland, College Park, MD 20742, USA.
  • Robert Gaskell
    Planetary Science Institute, 1700 East Fort Lowell, Suite 106, Tucson, AZ 85719, USA.
  • Timothy McCoy
    Department of Mineral Sciences, Smithsonian National Museum of Natural History, 10th and Constitution NW, Washington, DC 20560–0119, USA.
  • Andrew W. Beck
    Department of Mineral Sciences, Smithsonian National Museum of Natural History, 10th and Constitution NW, Washington, DC 20560–0119, USA.
  • Stefan E. Schröder
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Carle M. Pieters
    Department of Geological Sciences, Brown University, Providence, RI 02912, USA.
  • Kris J. Becker
    Astrogeology Science Center, U.S. Geological Survey, Flagstaff, AZ 86001, USA.
  • Bonnie J. Buratti
    Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
  • Brett Denevi
    Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA.
  • David T. Blewett
    Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA.
  • Ulrich Christensen
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Michael J. Gaffey
    Department of Space Studies, University of North Dakota, Grand Forks, ND 58202, USA.
  • Pablo Gutierrez-Marques
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Michael Hicks
    Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
  • Horst Uwe Keller
    Institut für Geophysik und extraterrestrische Physik, TU Braunschweig Mendelssohnstrasse 3, DE 38106 Braunschweig, Germany.
  • Thorsten Maue
    Max Planck Institute for Solar System Research, Max-Planck-Strasse 2, 37191 Katlenburg-Lindau, Germany.
  • Stefano Mottola
    Deutsches Zentrum für Luft und Raumfahrt (DLR)–German Aerospace Center, Institute of Planetary Research, Rutherfordstrasse 2, D-12489 Berlin, Germany.
  • Lucy A. McFadden
    NASA/Goddard Space Flight Center, Mail Code 160, Greenbelt, MD 20771, USA.
  • Harry Y. McSween
    Department of Earth and Planetary Sciences, University of Tennessee, 1412 Circle Drive, Knoxville, TN 37996–1410, USA.
  • David Mittlefehldt
    Astromaterials Research Office, NASA Johnson Space Center, Mail Code KR, Houston, TX 77058, USA.
  • David P. O’Brien
    Planetary Science Institute, 1700 East Fort Lowell, Suite 106, Tucson, AZ 85719, USA.
  • Carol Raymond
    Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
  • Christopher Russell
    Institute of Geophysics and Planetary Physics, University of California Los Angeles, Los Angeles, CA 90024–1567, USA.

書誌事項

公開日
2012-05-11
DOI
  • 10.1126/science.1219088
公開者
American Association for the Advancement of Science (AAAS)

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説明

<jats:title>A New Dawn</jats:title> <jats:p> Since 17 July 2011, NASA's spacecraft Dawn has been orbiting the asteroid Vesta—the second most massive and the third largest asteroid in the solar system (see the cover). <jats:bold> Russell <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="684" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1219381">684</jats:related-article> ) use Dawn's observations to confirm that Vesta is a small differentiated planetary body with an inner core, and represents a surviving proto-planet from the earliest epoch of solar system formation; Vesta is also confirmed as the source of the howardite-eucrite-diogenite (HED) meteorites. <jats:bold> Jaumann <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="687" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1219122">687</jats:related-article> ) report on the asteroid's overall geometry and topography, based on global surface mapping. Vesta's surface is dominated by numerous impact craters and large troughs around the equatorial region. <jats:bold> Marchi <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="690" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1218757">690</jats:related-article> ) report on Vesta's complex cratering history and constrain the age of some of its major regions based on crater counts. <jats:bold> Schenk <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="694" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1223272">694</jats:related-article> ) describe two giant impact basins located at the asteroid's south pole. Both basins are young and excavated enough amounts of material to form the Vestoids—a group of asteroids with a composition similar to that of Vesta—and HED meteorites. <jats:bold> De Sanctis <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="697" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1219270">697</jats:related-article> ) present the mineralogical characterization of Vesta, based on data obtained by Dawn's visual and infrared spectrometer, revealing that this asteroid underwent a complex magmatic evolution that led to a differentiated crust and mantle. The global color variations detailed by <jats:bold> Reddy <jats:italic>et al.</jats:italic> </jats:bold> (p. <jats:related-article xmlns:xlink="http://www.w3.org/1999/xlink" ext-link-type="doi" page="700" related-article-type="in-this-issue" vol="336" xlink:href="10.1126/science.1219088">700</jats:related-article> ) are unlike those of any other asteroid observed so far and are also indicative of a preserved, differentiated proto-planet. </jats:p>

収録刊行物

  • Science

    Science 336 (6082), 700-704, 2012-05-11

    American Association for the Advancement of Science (AAAS)

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