Updated on 2025/11/28

写真a

 
OTA Tsutomu
 
Organization
Institute for Planetary Materials Chief super technician
Position
Chief super technician
External link

Degree

  • 博士(理学) ( 新潟大学 )

Research Interests

  • geochemistry

  • Petrology

  • 地球化学

  • 岩石学

Research Areas

  • Natural Science / Solid earth sciences

Education

  • Niigata University   自然科学研究科   環境科学専攻

    1993.4 - 1996.3

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    Country: Japan

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  • Ehime University   理学研究科   地球科学専攻

    1991.3 - 1993.3

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    Country: Japan

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  • Ehime University   理学部   地球科学科

    1987.4 - 1991.3

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Research History

  • Okayama University   地球物質科学研究センター

    2004.1 - 2008.3

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  • Tokyo Institute of Technology   理学部

    2001.4 - 2003.12

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  • Tokyo Institute of Technology   理学部

    1997.4 - 2000.3

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Papers

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MISC

  • The Taitao ophiolite and related felsic plutonism nearby the Chile ridge subduction zone

    Anma ryo, Komiya Tsuyoshi, Kon Yoshiakai, Shibiya Takazou, Ota Tsutomu, Orihashi Yuji, Armstrong Richard

    Abstracts of Annual Meeting of the Geochemical Society of Japan   55   301 - 301   2008

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    Publisher:GEOCHEMICAL SOCIETY OF JAPAN  

    DOI: 10.14862/geochemproc.55.0.301.0

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  • Transportation of boron by subducting lithosphere; insights from diamondiferous tourmaline from Kokchetav

    Ota Tsutomu, Kobayashi Katsura, Nakamura Eizo

    Abstracts of Annual Meeting of the Geochemical Society of Japan   55   67 - 67   2008

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    Publisher:GEOCHEMICAL SOCIETY OF JAPAN  

    DOI: 10.14862/geochemproc.55.0.67.0

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  • O-142 Shuffled-cards structure of Kamuikotan high-P/T metamorphic rocks, central Hokkaido, Japan

    Sakakibara Masayuki, Yasumoto Kazumi, Ota Tsutomu, Ikeda Michiharu

    日本地質学会学術大会講演要旨   114   132 - 132   2007.9

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.2007.0.256.0

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  • S-47 Formation and Exhumation process of the Sanbagawa metamorphic belt, central Shikoku, Japan

    Aoki K., Masago H., Terabayashi M., Kaneko Y., Okamoto K., Yamamoto H., Ota T., Maruyama S.

    114   25 - 25   2007.9

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    Language:Japanese   Publisher:The Geological Society of Japan  

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  • Zircon geochemistry of Mid-Miocene adakites in the southern Patagonian province

    Tsutomu Ota

    Geochimica et Cosmochimica Acta   2003

  • O-12 Geology of the Taitao Ophiolite near the Chile Triple Junction

    Anma R., Veloso A., Kaneko Y., Terabayashi M., Ota T., Komiya T., Katayama I., Maruyama S., Herve F.

    Annual Meeting of the Geological Society of Japan   2002   7 - 7   2002

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.2002.0_7_2

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  • P-66 Stratigraphy of paleo-seamount limestone in the Cambrian accretionary complex in Gorny Altai mountain, southern Russia

    Uchio Y., Isozaki Y., Ota T., Utsunomiya A., Buslov M. M., Maruyama S.

    Annual Meeting of the Geological Society of Japan   2002   239 - 239   2002

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.2002.0_239_2

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  • P-68 The stratigraphy of Vendiian / Cambrian limestone derived from paleo-seamount in the Gomy Altai mountain, southern Russia

    Uchio Y, Isozaki Y, Kawahata H, Nohda S, Ota T, Buslov M. M, Maruyama S

    Annual Meeting of the Geological Society of Japan   2001 ( 0 )   231 - 231   2001

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.2001.0_231_2

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  • Metamorphic Petrology of Garnet Pyroxenite and Associated Gneiss from the Early Proterozoic Sharyzhalgai Block in the Southwestern Margin of Siberian Craton

    Ota, T., Sklyarov, E.V., Gladkochub, D.P., Watanabe, T.

    Gondwana Research   4 ( 4 )   2001

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  • O-126 The Cambrian limestone derived from paleo-seamount in the Gorny Altai mountain, southern Russia : Field occurrence, stratigraphy, radiometric age, microfossil and Carbon isotopic composition

    Uchio Y, Isozaki Y, Kawahata H, Nohda S, Ota T, Buslov M. M, Maruyama S

    Annual Meeting of the Geological Society of Japan   2000 ( 0 )   74 - 74   2000

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.2000.0_74_1

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  • Proterzoic-Phanerozoicboundary limestone in the Gorny Altai mountain, southern Russia : Lithology and Pb-Pbisotopic age

    Uchio Y., Isozaki Y., Nohda S., Ohta T, Ishikawa A., Utsunomiya A., Buslov M.M., Maruyama S.

    Annual Meeting of the Geological Society of Japan   1999   305 - 305   1999

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1999.0_305_2

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  • Geology of the Kokchetav UHP metamorphic belt, northern Kazakhstan (1)

    Kaneko Yoshiyuki, Maruyama Shigenori, Terabayashi Masaru, Yamamoto Hiroshi, Ishikawa Masahiro, Anma Ryo, Parkinson C.B, Ota Tsutomu, Nakajima Youichi, Katayama Ikuo, Yamauchi Kazuhiro, Masago Hideki, Ogasawara Toshihide

    Annual Meeting of the Geological Society of Japan   1998   431 - 431   1998

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1998.0_431

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  • Petrology of eclogite in Barchikol area, Kokchetav UHP belt, northern Kazakstan

    MASAGO Hideki, OTA Tsutomu, PARKINSON Chris, TERABAYASHI Masaru, NAKAJIMA Youichi, MARUYAMA Shigenori

    Annual Meeting of the Geological Society of Japan   1998   432 - 432   1998

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1998.0_432

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  • Vendian-Cambrian limestone in the Gorny Altai region, southern Russia:Field occurrence and lithology

    Uchio Yuko, Isozaki Yukio, Ohta Tsutomu, Maruyama Shigenori, Buslov Mikhail

    Annual Meeting of the Geological Society of Japan   1998   513 - 513   1998

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1998.0_513

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  • Petrology of greenstones from the Cambrian accretionary comprex, southern margin of Siberian Craton

    Utunomiya A., Ota T., Ishikawa A., Maruyama S., Buslov M.

    Annual Meeting of the Geological Society of Japan   1998   444 - 444   1998

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1998.0_444

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  • 198 On-going Orogeny (2) : Lithology and metamorphism of the eastern and western parts of the Timor-Tanimbar metamorphic belt,Eastern Indonesia

    Ota Tsutomu, Tsujimori Tatsuki, Kaneko Yoshiyuki, Kadarusman Ade, Okamoto Kazuaki, Maruyama Shigenori

    Annual Meeting of the Geological Society of Japan   1997   201   1997

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1997.0_201_1

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  • 181 Metamorphic zonation of the Proterozoic Capricorn orogen,western Australia

    Masago Hideki, Kaneko Yoshiyuki, Ohta Tsutomu, Maruyama Shigenori, Isozaki Yukio

    Annual Meeting of the Geological Society of Japan   1997   193 - 193   1997

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1997.0_193_1

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  • 197 On-going Orogeny (1) : Tectonic evolution of the Timor-Tanimbar metamorphic belt,Eastern Indonesia

    Kaneko Yoshiyuki, Maruyama Shigenori, Ota Tsutomu, Kadarusman Ade, Tsujimori Tatsuki, Okamoto Kazuaki

    Annual Meeting of the Geological Society of Japan   1997   200   1997

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1997.0_200_2

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  • 神居古潭変成帯の発達史-変形変成史に基づく白雲母K-Ar年代の再検討を踏まえて. 総合研究(A) : 日本列島のジュラ紀-古第三紀付加体形成における緑色岩の意義

    太田努

    研究報告   ( 1 )   51 - 68   1996

  • 390. Temporal development of thermal stucture and its controlling factors in a subduction zone : with an example of Kamuikotan subduction complex

    SAKAKIBARA Masayuki, OTA Tsutomu, NISHIKAWA Kiyoharu

    日本地質学会学術大会講演要旨   101   252 - 252   1994.9

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1994.0_252_1

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  • 低温高圧型変成岩の白雲母K-Ar年代の不一致-白雲母組成からのアプローチ-

    太田努

    日本地質学会第101年学術大会講演要旨   252   1994

  • 北海道, 旭川西方の神居古潭変成岩類の地質と変成作用

    太田努

    日本地質学会第99年学術大会演旨   477   1992

  • 40Ar-39Ar and K-Ar geochronological studies for Kamuikotan metamorphic rocks

    TAKIGAMI Yutaka, OHTA Tsutomu, SAKAKIBARA Masayuki

    Programme and abstracts the Volcanological Society of Japan   1991 ( 2 )   109 - 109   1991.10

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    Language:Japanese   Publisher:Volcanological Society of Japan  

    DOI: 10.18940/vsj.1991.2.0_109

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  • 304 K-Ar and Ar-Ar Ages of Kamuikotan Metamorphic Rocks, Hokkaido.

    Ohta Tsutomu, Sakakibara Masayuki, Itaya Tetsumaru, Takigami Yutaka

    日本地質学会学術大会講演要旨   98   435 - 435   1991.3

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    Language:Japanese   Publisher:The Geological Society of Japan  

    DOI: 10.14863/geosocabst.1991.0_435

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Research Projects

  • Spatiotemporal scale of isotope disequilibria in the mantle, deduced from lithium isotope compositions of mantle peridotite

    Grant number:17K05706  2017.04 - 2020.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)  Grant-in-Aid for Scientific Research (C)

    Ota Tsutomu

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    Grant amount:\4420000 ( Direct expense: \3400000 、 Indirect expense:\1020000 )

    The present study focused distributions of hydrogen and fluid-mobile elements including lithium isotopes in orogenic peridotites of the Horoman massif, Japan, to estimate spaciotemporal scales of mantle heterogeneity on light elements. The analytical results on the samples collected at various scales from kilometer (an entire massif) through meter (an outcrop) to submillimeter (a mineral) produced the following outcomes.
    The Horoman peridotites were partly affected at 150 Ma by a subduction-zone fluid. However in the core of the massif, they have retained geochemical characteristics derived from sub-seafloor hydrothermal alteration at 1 Ga. The hydrogen abundances are more than 10-times higher than those of a typical residual mantle. The presence of the Horoman massif suggests that ancient oceanic mantle domains formed by sub-seafloor hydrothermal alteration could have survived in the mantle for at least 1 Gy, and have influenced to dynamics and chemical evolution of the mantle.

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  • An integrated study of Paleoproterozoic high-pressure intermediate-type metamorphic belt: Implication for the operation of modern-style subduction processes

    Grant number:15H05212  2015.04 - 2018.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    Tsujimori Tatsuki

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    Grant amount:\15860000 ( Direct expense: \12200000 、 Indirect expense:\3660000 )

    High-pressure intermediate-type metamorphic belt surrounding the late Archean Tanzania Craton experienced Pacific-type subduction zone metamorphism in Orosirian Period at ca. 2 Ga. Epidote-amphibolite-facies meta-pillow basalts of the belt had a mid-ocean ridge basalt-like affinity. Details of eclogite- and high-pressure granulite-facies metamorphism has also brought new insight into Paleoproterozoic Pacific-type subduction processes.

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  • An integrated study of Paleo- and Neoproterozoic orogenic processes at the Tanzanian craton margin

    Grant number:24403010  2012.04 - 2015.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)  Grant-in-Aid for Scientific Research (B)

    TSUJIMORI Tatsuki, OTA Tsutomu, KOBAYASHI Katsura

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    Grant amount:\17160000 ( Direct expense: \13200000 、 Indirect expense:\3960000 )

    High-pressure metamorphic rocks occurring sporadically around the Archean Tanzanian craton record a crustal evolution related to Paleo- and Neoproterozoic orogeny. Our integrated studies confirmed that the Paleoproterozoic subduction-related units including eclogite-bearing high-pressure intermediate-type metamorphic belt and coeval paired granitic batholiths are overprinted significantly by a Pan-African granulite-facies regional metamorphism and deformation. The Pan-African events intrusions played the most important role in the crustal evolution.

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  • Water content and lithium isotope fractionation in subduction-zone mantle olivine

    Grant number:24540513  2012.04 - 2015.03

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)  Grant-in-Aid for Scientific Research (C)

    OTA Tsutomu, MALFAIT WIM J.

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    Grant amount:\5070000 ( Direct expense: \3900000 、 Indirect expense:\1170000 )

    In terms of lithium (Li) isotope fractionation between mantle olivine and aqueous fluid, we examined an interaction between mantle and surficial material, which has strongly affected the earth’s chemical evolution.
    Combining an experimental study in a simple system with Li-isotope analysis of natural mantle olivine revealed that the mantle olivine yielded Li isotopic abundances that fractionated by an interaction with aqueous fluid is relatively enriched in hydrogen, compared with the less fractionated ones.
    This result indicates that mantle materials that interacted with surficial materials have maintained their chemical characteristics including Li isotopic abundance, even under high temperature conditions in mantle on a geologic timescale. The mantle materials, interacted with surficial materials, have been transported back to the mantle by lithospheric plate subduction; such cycling has chemically differentiated the mantle and the surface, that is, the earth’s chemical evolution.

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  • 希ガス同位体を用いた「Old Rock Geochemistry」の展開

    Grant number:21244085  2009 - 2012

    日本学術振興会  科学研究費助成事業 基盤研究(A)  基盤研究(A)

    松本 拓也, 松田 准一, 辻森 樹, 太田 努, 山下 勝行, 宮川 千絵

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    Grant amount:\38220000 ( Direct expense: \29400000 、 Indirect expense:\8820000 )

    本年度は、中国東南部各地から採取したマントル捕獲岩の希ガス同位体分析を完了した。この地域の大陸下lithosphereは比較的最近に大規模な剥奪過程を経験したことが先行研究などにより提唱されており、希ガス同位体がどのような特徴を示すかで、大陸中央部のlithospbereの進化過程に制約条件を与えうると期待できる。分析した試料の特徴としては一様に希ガス含有量がオーストラリアで産出する同様の岩石と比べて少なく、結果として同位体分析もかなり困難であった。ヘリウムの同位体が典型的な上部マントルの億よりも10-20%低い億を示すものもあったため、比較的最近のガスの寄与というよりは、ある程度の期間マントル内で放射集変起源成分の蓄積された領域が存在し、その領域に起因する流体が付加されたものであると推定できる。また、インド洋意の玄武岩試料の分析も完了し中央インド洋海嶺のセグメント毎に明確なヘリウム同位体比の特徴の違いを発見した。一部のセグメントで明確にレユニオンマントルブルームに起因する成分の寄与を発見するとともに.あるセグメントでは上部マントルの値よりも低い3He/4Heが発見され、その様な値は脱ガスを経験した上部マントルがその後少なくとも1000万年以上の期間放射起線のヘリウムを蓄積し、その領域からのガスが特定のセグメントにヘリウムを供給する必要がある。上記2つの研究は対象は異なっているが、いずれも上部マントル内でのローカルな同位体進化を反映した同位体不均一の存在を示唆しており、地球内部の同位体進化を探る上で今後考慮すべき事柄である。また、一部のダイアモンドで見られるネオン同位体の特徴を解釈するために、ネオンの同位体進化曲線をモデル計算し論文として発表した。昨年度来から継続したオーストラリア東部の研究については論文を発表するとともに国際学会にて発表を行った。

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  • Behavior of lithium isotopes in subduction zone mantle

    Grant number:21540505  2009 - 2011

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)  Grant-in-Aid for Scientific Research (C)

    OTA Tsutomu, MORIGUCHI Takuya, KUNIHIRO Takuya, JAMES G. brophy

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    Grant amount:\4420000 ( Direct expense: \3400000 、 Indirect expense:\1020000 )

    This study aimed to decipher parameters of lithium partitioning and lithium isotope fractionation between mantle olivine and aqueous fluid, in terms of experimental petrology, in order to understand chemical interaction between surficial and mantle materials in deep subduction zone, which has defined a chemical evolution of the Earth. Lithium isotopic compositions obtained from synthesized olivines suggested that the subduction-zone mantle could have been more significantly fractionated in lithium isotope, rather than expected by previous studies.

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  • Experimental study on boron cycling in the upper mantle

    Grant number:18740346  2006 - 2008

    Japan Society for the Promotion of Science  Grants-in-Aid for Scientific Research Grant-in-Aid for Young Scientists (B)  Grant-in-Aid for Young Scientists (B)

    OOTA Tsutomu

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    Grant amount:\2980000 ( Direct expense: \2800000 、 Indirect expense:\180000 )

    地球という惑星の大部分はマントルで占められている.このマントルの活動によって形成された表層の物質は,プレート運動によって沈み込み帯からマントルへと戻っていく.その際,ある特定の化学成分は表層物質に濃集し,沈み込む際には表層物質から取り去られてマントルには戻ってこない.このような物質循環によって地球は進化してきた.本研究では,表層物質の沈み込み過程を高温高圧実験によって再現したり,マントル深部へ沈み込んだ岩石の化学組成を分析しりして,表層物質がマントル深部へ沈み込んでいく際に,ホウ素(およびリチウム)という元素がどのような挙動をするのかを明らかにし,地球マントルの化学進化の理解に貢献した.

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  • Chemical evolution of Earth through material differentiation at subduction zone

    2004

    Cooperative Research 

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    Grant type:Competitive

    With approaches from experimental petrology and petrography on natural samples, we attempt to quantify a series of parameters on chemical interactions between fluid and crustal and mantle materials at depths of subduction zone, and to decode chemical evolution of Earth

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  • 沈み込み帯における物質分化と地球の化学進化

    2004

    共同研究 

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    Grant type:Competitive

    実験岩石学的手法,および天然試料の記載岩石学を通じて,プレート沈み込み帯深部で進行する流体ー岩石間の化学的相互作用を定量化し,地球の大部分を占めるマントルの化学進化過程を明らかにする.

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  • 中生代の南太平洋スーパープルームの活動と環太平洋型高圧変成帯の上昇

    Grant number:97J04187  1998 - 1999

    日本学術振興会  科学研究費助成事業 特別研究員奨励費  特別研究員奨励費

    太田 努

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    Grant amount:\2400000 ( Direct expense: \2400000 )

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  • 広域変成帯の形成・上昇と太平洋型造山運動

    1996 - 2003

    共同研究 

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    Grant type:Competitive

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  • Regional metamorphism and Pacific-type orogeny

    1996 - 2003

    Cooperative Research 

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    Grant type:Competitive

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