The missing large impact craters on Ceres
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. Hiesinger and
C. T. Russell
Additional contact information
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
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
Nature Communications, 2016, vol. 7, issue 1, 1-9
Abstract:
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.
Date: 2016
References: Add references at CitEc
Citations:
Downloads: (external link)
https://www.nature.com/articles/ncomms12257 Abstract (text/html)
Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.
Export reference: BibTeX
RIS (EndNote, ProCite, RefMan)
HTML/Text
Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms12257
Ordering information: This journal article can be ordered from
https://www.nature.com/ncomms/
DOI: 10.1038/ncomms12257
Access Statistics for this article
Nature Communications is currently edited by Nathalie Le Bot, Enda Bergin and Fiona Gillespie
More articles in Nature Communications from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().