4.8 Article

The geomorphology, color, and thermal properties of Ryugu: Implications for parent-body processes

Journal

SCIENCE
Volume 364, Issue 6437, Pages 252-+

Publisher

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.aaw0422

Keywords

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Funding

  1. KAKENHI from the Japanese Society for Promotion of Science (JSPS) [JP25120006, 17H01175, JP17H06459, JP17K05639, JP16H04059, JP17KK0097, JP26287108, JP16H04044]
  2. JSPS Core-to-Core program International Network of Planetary Sciences
  3. French space agency CNES
  4. Complex Systems Academy of Excellence, IDEX JEDI of the Universite Cote d'Azur
  5. Space, Environment, Risk, and Resilience Academy of Excellence, IDEX JEDI of the Universite Cote d'Azur
  6. European Union's Horizon 2020 Research and Innovation Programme [687378]
  7. NASA Hayabusa2 Participating Scientist Program
  8. Center for Planetary Origin
  9. STFC [ST/S001271/1] Funding Source: UKRI
  10. Grants-in-Aid for Scientific Research [17H01175] Funding Source: KAKEN

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The near-Earth carbonaceous asteroid 162173 Ryugu is thought to have been produced from a parent body that contained water ice and organic molecules. The Hayabusa2 spacecraft has obtained global multicolor images of Ryugu. Geomorphological features present include a circum-equatorial ridge, east-west dichotomy, high boulder abundances across the entire surface, and impact craters. Age estimates from the craters indicate a resurfacing age of. 106 years for the top 1-meter layer. Ryugu is among the darkest known bodies in the Solar System. The high abundance and spectral properties of boulders are consistent with moderately dehydrated materials, analogous to thermally metamorphosed meteorites found on Earth. The general uniformity in color across Ryugu's surface supports partial dehydration due to internal heating of the asteroid's parent body.

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