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Spectrally blue hydrated parent body of asteroid (162173) Ryugu.

Eri TatsumiNaoya SakataniLucie RiuMoe MatsuokaRie HondaTomokatsu MorotaShingo KamedaTomoki NakamuraMichael ZolenskyRosario BrunettoTakahiro HiroiSho SasakiSei'ichiro WatanabeSatoshi TanakaJun TakitaCédric PilorgetJulia de LeónMarcel PopescuJuan Luis RizosJavier LicandroErnesto PalombaDeborah DomingueFaith VilasHumberto CampinsYuichiro ChoKazuo YoshiokaHirotaka SawadaYasuhiro YokotaMasahiko HayakawaManabu YamadaToru KouyamaHidehiko SuzukiChikatoshi HondaKazunori OgawaKohei KitazatoNaru HirataNaoyuki HirataYuichi TsudaMakoto YoshikawaTakanao SaikiFuyuto TeruiSatoru NakazawaYuto TakeiHiroshi TakeuchiYukio YamamotoTatsuaki OkadaYuri ShimakiKei ShiraiSeiji Sugita
Published in: Nature communications (2021)
Ryugu is a carbonaceous rubble-pile asteroid visited by the Hayabusa2 spacecraft. Small rubble pile asteroids record the thermal evolution of their much larger parent bodies. However, recent space weathering and/or solar heating create ambiguities between the uppermost layer observable by remote-sensing and the pristine material from the parent body. Hayabusa2 remote-sensing observations find that on the asteroid (162173) Ryugu both north and south pole regions preserve the material least processed by space weathering, which is spectrally blue carbonaceous chondritic material with a 0-3% deep 0.7-µm band absorption, indicative of Fe-bearing phyllosilicates. Here we report that spectrally blue Ryugu's parent body experienced intensive aqueous alteration and subsequent thermal metamorphism at 570-670 K (300-400 °C), suggesting that Ryugu's parent body was heated by radioactive decay of short-lived radionuclides possibly because of its early formation 2-2.5 Ma. The samples being brought to Earth by Hayabusa2 will give us our first insights into this epoch in solar system history.
Keyphrases
  • light emitting
  • ionic liquid