Characterization and genesis of mantle compositional hemispheres
Project/Area Number |
26247091
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Research Category |
Grant-in-Aid for Scientific Research (A)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Petrology/Mineralogy/Economic geology
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Research Institution | Japan Agency for Marine-Earth Science and Technology |
Principal Investigator |
Iwamori Hikaru 国立研究開発法人海洋研究開発機構, 地球内部物質循環研究分野, 分野長 (80221795)
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Co-Investigator(Kenkyū-buntansha) |
横山 哲也 東京工業大学, 理工学研究科, 准教授 (00467028)
中村 仁美 国立研究開発法人海洋研究開発機構, 地球内部物質循環研究分野, 研究員 (60572659)
石塚 治 国立研究開発法人産業技術総合研究所, 活断層・火山研究部門, 主任研究員 (90356444)
吉田 晶樹 国立研究開発法人海洋研究開発機構, 地球深部ダイナミクス研究分野, 主任研究員 (00371716)
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Co-Investigator(Renkei-kenkyūsha) |
Hanyu Takeshi 国立研究開発法人海洋研究開発機構, 地球内部物質循環研究分野, 主任研究員 (50359197)
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Research Collaborator |
Tatiana Churikova
Boris Gordeychik
Asobo Asaah
Festus T. Aka
Shimizu Kenji
Nishizawa Tatsuji
Ozawa Takahiro
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Project Period (FY) |
2014-04-01 – 2017-03-31
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Project Status |
Completed (Fiscal Year 2016)
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Budget Amount *help |
¥42,510,000 (Direct Cost: ¥32,700,000、Indirect Cost: ¥9,810,000)
Fiscal Year 2016: ¥8,710,000 (Direct Cost: ¥6,700,000、Indirect Cost: ¥2,010,000)
Fiscal Year 2015: ¥8,580,000 (Direct Cost: ¥6,600,000、Indirect Cost: ¥1,980,000)
Fiscal Year 2014: ¥25,220,000 (Direct Cost: ¥19,400,000、Indirect Cost: ¥5,820,000)
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Keywords | マントル / 組成 / 同位体 / 半球構造 / 統計解析 / 独立成分分析 / 水 / 物質循環 / 南太平洋 / カムチャッカ / 不均質構造 / 対流 / カメルーン |
Outline of Final Research Achievements |
Geochemical heterogeneity in the Earth’s mantle has been investigated based on the Quaternary basalts over the globe. With a special attention to recently proposed “east-west mantle geochemical hemispheres”, (1) detailed inspection along the hemisphere boundary, (2) Independent Component Analysis of global geochemical data, and (3) numerical simulation of water-bearing mantle convection have been performed. As a result, it has been revealed that (A) the eastern hemisphere is relatively enriched in hydrophile components, and (B) the hemispherical structure extends from the near-surface to the inner core via “top-down hemispherical dynamics” in which the supercontinent and focused subduction towards it could have created the global hemispherical structure.
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Report
(4 results)
Research Products
(17 results)
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[Journal Article] Geochemistry of lavas from maar-bearing volcanoes in the Oku Volcanic Group of the Cameroon Volcanic Line2015
Author(s)
A.N.E. Asaah, T. Yokoyama, F.T. Aka, T. Usui, T. Kuritani, M.J. Wirmvem, H. Iwamori, E.M. Fozing, J. Tamen, G.Z. Mofor, T. Ohba, G. Tanyileke, and J.V. Hell.
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Journal Title
Chemical Geology
Volume: 印刷中
Pages: 55-69
DOI
Related Report
Peer Reviewed
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[Presentation] Subduction Processes and a New Hypothesis for ``Top-down Hemispherical Dynamics of the2014
Author(s)
Hikaru Iwamori, Hitomi Nakamura, Takeshi hanyu, Junichi Kimura, Tomoeki Nakakuki, Takashi Nakagawa, Masaki Yoshida, Satoru Tanaka, Daisuke Suetsugu, Masayuki Obayashi
Organizer
日本地球惑星科学連合2014年大会
Place of Presentation
Pacifico Yokohama, 神奈川県横浜市
Year and Date
2014-04-28
Related Report
Int'l Joint Research / Invited