Author
Listed:
- S. Marchi
(Southwest Research Institute)
- A. I. Ermakov
(Massachusetts Institute of Technology)
- C. A. Raymond
(Jet Propulsion Laboratory, California Institute of Technology)
- R. R. Fu
(Lamont-Doherty Earth Observatory, Columbia University)
- D. P. O’Brien
(Planetary Science Institute)
- M. T. Bland
(USGS Astrogeology Science Center)
- E. Ammannito
(University of California)
- M. C. De Sanctis
(Istituto di Astrofisica e Planetologia Spaziali, INAF)
- T. Bowling
(University of Chicago)
- P. Schenk
- J. E. C. Scully
(Jet Propulsion Laboratory, California Institute of Technology)
- D. L. Buczkowski
(John Hopkins Applied Physics Laboratory)
- D. A. Williams
(School of Earth and Space Exploration, Arizona State University)
- H. Hiesinger
(Institut für Planetologie, Westfälische Wilhelms-Universität)
- C. T. Russell
(University of California)
Abstract
Asteroids provide fundamental clues to the formation and evolution of planetesimals. Collisional models based on the depletion of the primordial main belt of asteroids predict 10–15 craters >400 km should have formed on Ceres, the largest object between Mars and Jupiter, over the last 4.55 Gyr. Likewise, an extrapolation from the asteroid Vesta would require at least 6–7 such basins. However, Ceres’ surface appears devoid of impact craters >∼280 km. Here, we show a significant depletion of cerean craters down to 100–150 km in diameter. The overall scarcity of recognizable large craters is incompatible with collisional models, even in the case of a late implantation of Ceres in the main belt, a possibility raised by the presence of ammoniated phyllosilicates. Our results indicate that a significant population of large craters has been obliterated, implying that long-wavelength topography viscously relaxed or that Ceres experienced protracted widespread resurfacing.
Suggested Citation
S. Marchi & A. I. Ermakov & C. A. Raymond & R. R. Fu & D. P. O’Brien & M. T. Bland & E. Ammannito & M. C. De Sanctis & T. Bowling & P. Schenk & J. E. C. Scully & D. L. Buczkowski & D. A. Williams & H., 2016.
"The missing large impact craters on Ceres,"
Nature Communications, Nature, vol. 7(1), pages 1-9, November.
Handle:
RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms12257
DOI: 10.1038/ncomms12257
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