2012 Fiscal Year Final Research Report
Study of crustal formation mechanism and origin of dichotomy of the Moon
Project/Area Number |
22540443
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Solid earth and planetary physics
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Research Institution | Japan Aerospace Exploration Agency |
Principal Investigator |
OHTAKE Makiko 独立行政法人宇宙航空研究開発機構, 宇宙科学研究所, 助教 (30373442)
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Project Period (FY) |
2010 – 2012
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Keywords | かぐや / 月 / 地殻 / 惑星起 / 進化 / 惑星探査 |
Research Abstract |
This study apply an empirical algorithm to lunar reflectance spectra from the Kaguya and report that magnesium contents relative to iron of primitive crustal highland rocks on the farside are higher than on the nearside. Our findings indicate that the farside crust consists of rocks that crystallized from less-evolved magma than the nearside crust. This indicates that the lunar dichotomy is directly linked to crystallization of the magma ocean and suggests that the composition of the magma ocean was more primitive at the time of crustal growth than previously estimated.
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[Journal Article] 2012, Asymmetric crustal growth on the Moon indicated by primitive farside highland materials2012
Author(s)
Makiko Ohtake, Hiroshi Takeda, Tsuneo Matsunaga, Yasuhiro Yokota, Junichi Haruyama,Tomokatsu Morota, Satoru Yamamoto, Yoshiko Ogawa, Takahiro Hiroi, Yuzuru Karouji,Kazuto Saiki, Paul G. Lucey,
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Journal Title
Nature Geoscience
Volume: 5
Pages: 384-388
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[Presentation] 月高地地殻の化学組成から推定する高地地殻形成過程2012
Author(s)
大竹真紀子,武田弘,松永恒雄,横田康弘,春山純一,諸田智克,石原吉明,山本聡,小川佳子,廣井孝弘,唐牛譲,佐伯和人
Organizer
日本惑星科学会 日本惑星科学会2012年度秋季講演会
Place of Presentation
神戸大学
Year and Date
20121024-26
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[Presentation] かぐや分光データを用いた月高地地殻の鉱物量比とMg#の深さ方向変化2012
Author(s)
大竹真紀子,武田弘,松永恒雄,横田康弘,春山純一,諸田智克,石原吉明,山本聡,小川佳子,廣井孝弘,唐牛譲,佐伯和人
Organizer
Japan Geoscience Union Japan Geoscience Union Meeting 2012
Place of Presentation
幕張メッセ
Year and Date
20120520-25
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