TY - JOUR
T1 - Adhering grains and surface features on two Itokawa particles Space science Science of solar system materials examined from Hayabusa and future missions (II)
AU - Dobricə, E.
AU - Ogliore, R. C.
N1 - Publisher Copyright:
© 2016 Dobricə and Ogliore.
PY - 2016/12/1
Y1 - 2016/12/1
N2 - We investigated the surface texture and chemical compositions of two ~40-μm particles returned from the surface regolith of asteroid Itokawa (RB-DQ04-0062 and RB-DQ04-0091) by the Japan Aerospace Exploration Agency's Hayabusa mission. We identified splash melts, surface blistering, and many small adhering particles. Seven focused ion beam sections were extracted from both Itokawa particles, targeting one splash melt and ten adhering particles to investigate their composition and provenance and the role of micrometeoroid impacts on Itokawa's surface. Based on the particle's structure, mineralogy, and interface between the adhering particle and host grain, we identified lithic fragments and particles deposited by impact. These have morphologies and compositions consistent with impact-generated deposits: two have morphologies and compositions that are consistent with impact-generated silica glass, and one was a Ni-free, metallic Fe, and S-rich assemblage that was likely generated by vapor recondensation during a micrometeoroid impact. This study shows that, even though its regolith is young, micrometeoroid impacts have altered the regolith of asteroid Itokawa.
AB - We investigated the surface texture and chemical compositions of two ~40-μm particles returned from the surface regolith of asteroid Itokawa (RB-DQ04-0062 and RB-DQ04-0091) by the Japan Aerospace Exploration Agency's Hayabusa mission. We identified splash melts, surface blistering, and many small adhering particles. Seven focused ion beam sections were extracted from both Itokawa particles, targeting one splash melt and ten adhering particles to investigate their composition and provenance and the role of micrometeoroid impacts on Itokawa's surface. Based on the particle's structure, mineralogy, and interface between the adhering particle and host grain, we identified lithic fragments and particles deposited by impact. These have morphologies and compositions consistent with impact-generated deposits: two have morphologies and compositions that are consistent with impact-generated silica glass, and one was a Ni-free, metallic Fe, and S-rich assemblage that was likely generated by vapor recondensation during a micrometeoroid impact. This study shows that, even though its regolith is young, micrometeoroid impacts have altered the regolith of asteroid Itokawa.
KW - Asteroid
KW - Micrometeoroid
KW - Regolith
KW - Space weathering
UR - https://www.scopus.com/pages/publications/84958213682
U2 - 10.1186/s40623-016-0391-7
DO - 10.1186/s40623-016-0391-7
M3 - Article
AN - SCOPUS:84958213682
SN - 1343-8832
VL - 68
JO - Earth, Planets and Space
JF - Earth, Planets and Space
IS - 1
M1 - 21
ER -