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Microstructural and chemical features of impact melts on Ryugu particle surfaces: Records of interplanetary dust hit on asteroid Ryugu.
Matsumoto, Megumi; Matsuno, Junya; Tsuchiyama, Akira; Nakamura, Tomoki; Enokido, Yuma; Kikuiri, Mizuha; Nakato, Aiko; Yasutake, Masahiro; Uesugi, Kentaro; Takeuchi, Akihisa; Enju, Satomi; Okumura, Shota; Mitsukawa, Itaru; Sun, Mingqi; Miyake, Akira; Haruta, Mitsutaka; Igami, Yohei; Yurimoto, Hisayoshi; Noguchi, Takaaki; Okazaki, Ryuji; Yabuta, Hikaru; Naraoka, Hiroshi; Sakamoto, Kanako; Tachibana, Shogo; Zolensky, Michael; Yada, Toru; Nishimura, Masahiro; Miyazaki, Akiko; Yogata, Kasumi; Abe, Masanao; Okada, Tatsuaki; Usui, Tomohiro; Yoshikawa, Makoto; Saiki, Takanao; Tanaka, Satoshi; Terui, Fuyuto; Nakazawa, Satoru; Watanabe, Sei-Ichiro; Tsuda, Yuichi.
Afiliação
  • Matsumoto M; Department of Earth and Planetary Materials Sciences, Tohoku University, Miyagi 980-8578, Japan.
  • Matsuno J; Research Organization of Science and Technology, Ritsumeikan University, Shiga 525-8577, Japan.
  • Tsuchiyama A; Research Organization of Science and Technology, Ritsumeikan University, Shiga 525-8577, Japan.
  • Nakamura T; Chinese Academy of Sciences (CAS) Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, CAS, Guangzhou 510640, China.
  • Enokido Y; CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China.
  • Kikuiri M; Department of Earth and Planetary Materials Sciences, Tohoku University, Miyagi 980-8578, Japan.
  • Nakato A; Department of Earth and Planetary Materials Sciences, Tohoku University, Miyagi 980-8578, Japan.
  • Yasutake M; Department of Earth and Planetary Materials Sciences, Tohoku University, Miyagi 980-8578, Japan.
  • Uesugi K; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Takeuchi A; Research and Utilization Division, Japan Synchrotron Radiation Research Institute (JASRI/SPring-8), Hyogo 679-5198, Japan.
  • Enju S; Research and Utilization Division, Japan Synchrotron Radiation Research Institute (JASRI/SPring-8), Hyogo 679-5198, Japan.
  • Okumura S; Research and Utilization Division, Japan Synchrotron Radiation Research Institute (JASRI/SPring-8), Hyogo 679-5198, Japan.
  • Mitsukawa I; Earth's Evolution and Environment Course, Department of Mathematics, Physics, and Earth Science, Ehime University, Ehime 790-8577, Japan.
  • Sun M; Division of Earth and Planetary Sciences, Kyoto University, Kyoto 606-8502, Japan.
  • Miyake A; Division of Earth and Planetary Sciences, Kyoto University, Kyoto 606-8502, Japan.
  • Haruta M; Chinese Academy of Sciences (CAS) Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, CAS, Guangzhou 510640, China.
  • Igami Y; CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China.
  • Yurimoto H; Division of Earth and Planetary Sciences, Kyoto University, Kyoto 606-8502, Japan.
  • Noguchi T; Institute for Chemical Research, Kyoto University, Gokasho, Uji, Kyoto 611-0011, Japan.
  • Okazaki R; Division of Earth and Planetary Sciences, Kyoto University, Kyoto 606-8502, Japan.
  • Yabuta H; Department of Natural History Sciences, Hokkaido University, Sapporo 060-0810, Japan.
  • Naraoka H; Division of Earth and Planetary Sciences, Kyoto University, Kyoto 606-8502, Japan.
  • Sakamoto K; Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 819-0395, Japan.
  • Tachibana S; Graduate School of Advanced Science and Engineering, Hiroshima University, Higashi-HiroshimaHiroshima 739-8526, Japan.
  • Zolensky M; Department of Earth and Planetary Sciences, Kyushu University, Fukuoka 819-0395, Japan.
  • Yada T; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Nishimura M; Department of Earth and Planetary Science, The University of Tokyo, Tokyo 113-0033, Japan.
  • Miyazaki A; NASA Johnson Space Center, Houston, TX 77058, USA.
  • Yogata K; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Abe M; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Okada T; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Usui T; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Yoshikawa M; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Saiki T; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Tanaka S; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Terui F; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Nakazawa S; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Watanabe SI; Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA), Sagamihara 252-5210, Japan.
  • Tsuda Y; Department of Mechanical Engineering, Kanagawa Institute of Technology, Atsugi 243-0292, Japan.
Sci Adv ; 10(3): eadi7203, 2024 Jan 19.
Article em En | MEDLINE | ID: mdl-38241366
ABSTRACT
The Hayabusa2 spacecraft delivered samples of the carbonaceous asteroid Ryugu to Earth. Some of the sample particles show evidence of micrometeoroid impacts, which occurred on the asteroid surface. Among those, particles A0067 and A0094 have flat surfaces on which a large number of microcraters and impact melt splashes are observed. Two impact melt splashes and one microcrater were analyzed to unveil the nature of the objects that impacted the asteroid surface. The melt splashes consist mainly of Mg-Fe-rich glassy silicates and Fe-Ni sulfides. The microcrater trapped an impact melt consisting mainly of Mg-Fe-rich glassy silicate, Fe-Ni sulfides, and minor silica-rich glass. These impact melts show a single compositional trend indicating mixing of Ryugu surface materials and impactors having chondritic chemical compositions. The relict impactor in one of the melt splashes shows mineralogical similarity with anhydrous chondritic interplanetary dust particles having a probable cometary origin. The chondritic micrometeoroids probably impacted the Ryugu surface during its residence in a near-Earth orbit.

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Adv Ano de publicação: 2024 Tipo de documento: Article País de afiliação: Japão

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Adv Ano de publicação: 2024 Tipo de documento: Article País de afiliação: Japão