2009 Fiscal Year Final Research Report
Mass transfer from amphibolite-facies slab to the mantle and magma genesis in the initial stage of subduction
Project/Area Number |
18340171
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Research Category |
Grant-in-Aid for Scientific Research (B)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Japan Agency for Marine-Earth Science and Technology |
Principal Investigator |
ISHIKAWA Tsuyoshi Japan Agency for Marine-Earth Science and Technology, 高知コア研究所, グループリーダー (30270979)
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Project Period (FY) |
2006 – 2009
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Keywords | オマーンオフィオライト / 島弧 / 火山岩 / ボニナイト / 微量元素 / 同位体 / マグマ / 流体 |
Research Abstract |
Field survey and chemical analysis were carried out for the Oman ophiolite, a large fragment of 100 million year-old oceanic lithosphere. The field survey revealed widespread occurrence of boninite which represents the volcanic rock formed in subduction zone with extremely hot thermal structure. The chemical analysis showed that hydrous fluids liberated from subducted, amphibolite-facies oceanic crust (500~700℃) were widely incorporated in magma genesis in the initial stage of subduction.
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[Journal Article] Browning, E.-L., Li, X., and The IODP Expedition 307 Scientists, Age constraints on the origin and growth history of a deep-water coral mound in NE Atlantic drilled in IODP Expedition 307.2007
Author(s)
Kano, A., Ferdelman, T.G., Williams, T., Henriet, J.-P., Ishikawa, T., Kawagoe, N., Takashima, C., Kakizaki, Y., Abe, K., Sakai, S.
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Journal Title
Geology 35
Pages: 1051-1054
Peer Reviewed
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[Remarks] 永石一弥,Fluid transfer and magmatism in the initial stage of subduction: Inference from the Oman ophiolite(沈み込み帯形成最初期の流体移動とマグマ形成過程:オマーンオフィオライトからの推定).博士論文,静岡大学大学院理工学研究科環境科学専攻,2009年3月
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[Remarks] 山岡香子, Study on hydrothermal alteration of oceanic crust in the Oman ophiolite based on isotope geochemistry(同位体地球化学に基づくオマーンオフィオライト海洋地殻の熱水変質).博士論文,東京大学大学院新領域創生科学研究科自然環境学専攻,2010年3月