Understanding the geological modification processes on asteroids is fundamental for elucidating their surface evolution. Images of small asteroids from spacecrafts show a depletion in smaller craters. Seismic shaking was considered to be responsible for erasing such small craters and the main driver modifying the geology of asteroids. However,...
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2022 (v1)Journal articleUploaded on: December 3, 2022
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December 2020 (v1)Journal article
International audience
Uploaded on: December 4, 2022 -
2021 (v1)Journal article
Recent asteroid missions have revealed that many sub-kilometer asteroids are rubble piles. Large parts of their surfaces are covered with boulders larger than tens of centimeters. An evaluation of the abundance and size distribution of boulders provides clues to understand surface processes on boulder-covered asteroids. Here we report a new...
Uploaded on: December 4, 2022 -
March 20, 2019 (v1)Journal article
International audience
Uploaded on: December 4, 2022 -
2022 (v1)Journal article
Martian moons exploration, MMX, is the new sample return mission planned by the Japan Aerospace Exploration Agency (JAXA) targeting the two Martian moons with the scheduled launch in 2024 and return to the Earth in 2029. The major scientific objectives of this mission are to determine the origin of Phobos and Deimos, to elucidate the early...
Uploaded on: December 3, 2022 -
November 2021 (v1)Journal article
Many small boulders with reflectance values higher than 1.5 times the average reflectance have been found on the near-Earth asteroid 162,173 Ryugu. Based on their visible wavelength spectral differences, Tatsumi et al.
Uploaded on: December 4, 2022 -
November 2021 (v1)Journal article
Many small boulders with reflectance values higher than 1.5 times the average reflectance have been found on the near-Earth asteroid 162,173 Ryugu. Based on their visible wavelength spectral differences, Tatsumi et al.
Uploaded on: December 4, 2022 -
2020 (v1)Journal article
Carbonaceous (C-type) asteroids1 are relics of the early Solar System that have preserved primitive materials since their formation approximately 4.6 billion years ago. They are probably analogues of carbonaceous chondrites2,3 and are essential for understanding planetary formation processes. However, their physical properties remain poorly...
Uploaded on: December 4, 2022