Updated on 2025/06/07

写真a

 
TAKAZAWA Eiichi
 
Organization
Academic Assembly Institute of Science and Technology CHIKYU SEIBUTSU KAGAKU KEIRETU Professor
Faculty of Science Professor
Graduate School of Science and Technology Environmental Science and Technology Professor
Title
Professor
External link

Degree

  • Ph.D. ( 1996.9   Massachusetts Institute of Technology )

Research Interests

  • マントル岩石学

Research Areas

  • Natural Science / Solid earth sciences

Research History (researchmap)

  • Japan Agency for Marine-Earth Science and Technology   Guest Researcher

    2021.4 - 2024.3

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  • Japan Agency for Marine-Earth Science and Technology   Visiting Principal Researcher

    2014.4 - 2021.3

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  • Niigata University   Faculty of Science   Professor

    2013.5

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    Country:Japan

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  • Niigata University   Graduate School of Science and Technology   Professor

    2013.5

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    Country:Japan

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  • Niigata University   Faculty of Science   Associate Professor

    2004.4 - 2013.4

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    Country:Japan

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  • Niigata University   Faculty of Science   Associate Professor (as old post name)

    1999.10 - 2004.3

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    Country:Japan

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  • Niigata University   Faculty of Science   Lecturer

    1997.10 - 1999.9

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    Country:Japan

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Research History

  • Niigata University   Professor

    2013.5

  • Niigata University   Graduate School of Science and Technology Environmental Science and Technology   Professor

    2013.5

  • Niigata University   Graduate School of Science and Technology Environmental Science and Technology   Professor

    2013.5

  • Niigata University   Faculty of Science Department of Geology   Professor

    2013.5 - 2017.3

  • Niigata University   Faculty of Science Department of Geology   Associate Professor

    2004.4 - 2013.4

  • Niigata University   Faculty of Science   Lecturer

    1997.1 - 1999.9

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Education

  • Massachusetts Institute of Technology   Department of Earth, Atmospheric and Planetary Sciences

    1990.9 - 1996.6

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    Country: United States

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  • Kumamoto University   Graduate School of Science and Technology   環境科学専攻

    1989.4 - 1995.3

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    Country: Japan

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  • Hokkaido University   大学院理学研究科   地質学鉱物学専攻

    1987.4 - 1989.3

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    Country: Japan

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  • Hokkaido University   School of Science   地質学鉱物学科

    1982.4 - 1986.3

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    Country: Japan

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Papers

  • Variable Upper Mantle Geochemical Processes Constrained From Independent Component Analysis of the Fizh Massif, Northern Oman Ophiolite

    Yuto Miki, Eiichi Takazawa, Kenta Ueki, Tatsu Kuwatani

    Geochemistry, Geophysics, Geosystems   2025.3

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1029/2024GC012134

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  • Petrogenesis and tectonic evolution of mineralized mafic intrusions in the Eastern Desert of Egypt: Implications for gold–sulfide genesis

    Mohamed Zaki Khedr, Mohamed H. Ghoneim, Weal Hagag, Christoph Hauzenberger, Akihiro Tamura, Yuji Ichiyama, Eiichi Takazawa, Ali Y. Kahal, Kamal Abdelrahman, Sara Zamzam, Tomoaki Morishita, Amr El-Awady

    Ore Geology Reviews   173   2024.10

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1016/j.oregeorev.2024.106273

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  • Mineralogy and Geochemistry of Titaniferous Iron Ores in El-Baroud Layered Gabbros: Fe-Ti Ore Genesis and Tectono-Metallogenetic Setting

    Mohamed Zaki Khedr, Ahmed Moftah, N. H. El-Shibiny, Akihiro Tamura, Wei Tan, Yuji Ichiyama, Eiichi Takazawa, Ali Y. Kahal, Kamal Abdelrahman

    Minerals   14 ( 7 )   2024.7

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.3390/min14070679

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  • Mineralogy and Geochemistry of Jasperoid Veins in Neoproterozoic Metavolcanics: Evidence of Silicification, Pyritization and Hematization

    Mohamed Zaki Khedr, Mahmoud A. Sayed, Shehata Ali, Mokhles K. Azer, Yuji Ichiyama, Eiichi Takazawa, Ali Y. Kahal, Kamal Abdelrahman, Ali M. Mahdi

    Minerals   14 ( 7 )   2024.7

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.3390/min14070647

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  • Genesis of Rare Metal Granites in the Nubian Shield: Tectonic Control and Magmatic and Metasomatic Processes

    Mohamed Zaki Khedr, Saif M. Abo Khashaba, Eiichi Takazawa, Safaa M. Hassan, Mokhles K. Azer, N. H. El-Shibiny, Kamal Abdelrahman, Yuji Ichiyama

    Minerals   2024.5

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.3390/min14050522

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  • The Geology and Mineral Chemistry of Beryl Mineralization, South Eastern Desert, Egypt: A Deeper Insight into Genesis and Distribution

    Prof. Mohamed Khedr, Gehad M. Saleh, Abdelfadil, K. M., Eiichi Takazawa, kamal Hassanein, Akihiro Tamura, Shaimaa Ali El-Shafei

    Minerals   2024.4

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.3390/min14050465

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  • The magnesium isotopic composition of the mantle

    Xiao-Ning Liu, Remco C. Hin, Christopher D. Coath, Michael Bizimis, Li Su, Dmitri A. Ionov, Eiichi Takazawa, Richard Brooker, Tim Elliott

    Geochimica et Cosmochimica Acta   2023.10

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1016/j.gca.2023.08.011

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  • Remote sensing and geochemical investigations of sulfide-bearing metavolcanic and gabbroic rocks (Egypt): Constraints on host-rock petrogenesis and sulfide genesis

    Mohamed Zaki Khedr, Samir Kamh, Ahmed A. Al Desouky, Eiichi Takazawa, Christoph Hauzenberger, Scott A. Whattam, Amr El-Awady

    Gondwana Research   2023.7

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1016/j.gr.2023.03.021

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  • Integration of remote sensing and geochemical data to characterize mineralized A-type granites, Egypt: implications for origin and concentration of rare metals

    Mohamed Zaki Khedr, Saif M. Abo Khashaba, N. H. El-Shibiny, Eiichi Takazawa, Safaa M. Hassan, Mokhles K. Azer, Scott A. Whattam, Reda A. El-Arafy, Yuji Ichiyama

    International Journal of Earth Sciences   2023.6

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    Publishing type:Research paper (scientific journal)   Publisher:Springer Science and Business Media LLC  

    DOI: 10.1007/s00531-023-02323-4

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    Other Link: https://link.springer.com/article/10.1007/s00531-023-02323-4/fulltext.html

  • Application of remote sensing data integration in detecting mineralized granitic zones: A case study of the Gabal Al-Ijlah Al-Hamra, Central Eastern Desert, Egypt

    Saif M. Abo Khashaba, N.H. El-Shibiny, Safaa M. Hassan, Eiichi Takazawa, Mohamed Zaki Khedr

    Journal of African Earth Sciences   200   104855 - 104855   2023.4

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    Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.jafrearsci.2023.104855

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  • Genesis and evaluation of heavy minerals in black sands: A case study from the southern Eastern Desert of Egypt Reviewed

    Mohamed Zaki Khedr, Hamada Zaghloul, Eiichi Takazawa, Hesham El-Nahas, Mokhles K. Azer, Shaimaa Ali El-Shafei

    Geochemistry   83 ( 1 )   125945 - 125945   2023.4

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    Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.chemer.2022.125945

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  • Preface: Special Issue on Ophiolites and Oceanic Lithosphere

    Peter B. Kelemen, Jürg M. Matter, Damon A.H. Teagle, Jude A. Coggon, Marguerite Godard, Katsuyoshi Michibayashi, Eiichi Takazawa, Alexis S. Templeton, Ken Williams, Zaher Al Sulaimani

    Journal of Geophysical Research: Solid Earth   128 ( 4 )   2023.4

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1029/2023JB026677

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  • The cadmium and zinc isotope compositions of the silicate Earth – Implications for terrestrial volatile accretion Reviewed

    Harvey Pickard, Emeliana Palk, Maria Schönbächler, Rebekah E.T. Moore, Barry J. Coles, Katharina Kreissig, Katrina Nilsson-Kerr, Samantha J. Hammond, Eiichi Takazawa, Christophe Hémond, Peter Tropper, Dan N. Barfod, Mark Rehkämper

    Geochimica et Cosmochimica Acta   338   165 - 180   2022.12

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    Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.gca.2022.09.041

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  • Remote sensing techniques and geochemical constraints on the formation of the Wadi El-Hima mineralized granites, Egypt: new insights into the genesis and accumulation of garnets Reviewed

    Mohamed Zaki Khedr, Saif M. Abo Khashaba, N. H. El-Shibiny, Reda A. El-Arafy, Eiichi Takazawa, Mokhles K. Azer, Richard. M. Palin

    International Journal of Earth Sciences   111 ( 7 )   2409 - 2443   2022.10

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    Publishing type:Research paper (scientific journal)   Publisher:Springer Science and Business Media LLC  

    Abstract

    The Wadi El-Hima Neoproterozoic I- and A-type granites in the Southern Eastern Desert of Egypt are rich in garnets (up to 30 vol%) and are cut by NW–SE strike-slip faults, as confirmed from structure lineament extraction maps. These mineralized granites and garnet mineralization zones can be successfully discriminated using remote sensing techniques. Spectral angle mapper and matched filtering techniques are highly effective for mapping garnet-rich zones and show that the highest garnet concentrations occur along the intrusive contact zone of NW–SE striking faults. El-Hima granites have high SiO<sub>2</sub> (73.5–75.1 wt%), Al<sub>2</sub>O<sub>3</sub> (13.4–15.3 wt%) and total alkali (6.7–8.7 wt%) contents, suggesting that they were sourced from peraluminous (A/CNK &gt; 1) parental magmas. Garnet-bearing trondhjemites are metasomatic in origin and formed after I-type tonalite-granodiorites, which originated in a volcanic arc tectonic setting. Garnet-rich syenogranites and alkali-feldspar granites are both post-collisional A-type granites: the syenogranites formed from peraluminous magmas generated by partial melting of lower crustal tonalite and metasedimentary protoliths during lithospheric delamination, and the alkali-feldspar granites crystallized from highly fractionated, felsic and alkali-rich peraluminous magmas in the upper crust. Garnets in El-Hima mineralized granites occur in three forms: (1) subhedral disseminated crystals, (2) vein-type crystals, and (3) aggregated subhedral crystals, reflecting different mechanisms of accumulation. All are dominantly almandine in composition (Alm<sub>76</sub>Sps<sub>10</sub> Prp<sub>7</sub>Grs<sub>6</sub>Adr<sub>1</sub>) and have high average concentrations of heavy rare earth elements (HREE) (ΣHREE = 1636 ppm), Y = (3394 ppm), Zn (325 ppm), Li (39.17 ppm) and Ga (34.94 ppm). Garnet REE patterns show strong negative Eu anomalies with HREE enriched relative to LREE, indicating a magmatic origin. These magmatic garnets are late-stage crystallization products of Al-rich hydrous magmas, and formed at low temperature (680–730 °C) and pressure (2.1–2.93 kbar) conditions in the upper continental crust. Peculiar garnet concentrations in syenogranites near and along contact zones with alkali feldspar granites are related to peraluminous parent hydrous magma compositions. These garnets formed by in situ crystallization from A-type granite melts, alongside accumulation of residual garnets left behind after partial melting of the host garnet-rich granites along the intrusive contact. Magmatic-fluid flow along the NW–SE striking fault of Najd system enhanced garnet accumulation in melts, which formed clots and veins of garnet.

    DOI: 10.1007/s00531-022-02237-7

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    Other Link: https://link.springer.com/article/10.1007/s00531-022-02237-7/fulltext.html

  • Styles of Fe–Ti–V ore deposits in the Neoproterozoic layered mafic-ultramafic intrusions, south Eastern Desert of Egypt: Evidence for fractional crystallization of V-rich melts Reviewed

    Mohamed Zaki Khedr, Eiichi Takazawa, Shoji Arai, Robert J. Stern, Tomoaki Morishita, Amr El-Awady

    Journal of African Earth Sciences   194   104620 - 104620   2022.10

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    DOI: 10.1016/j.jafrearsci.2022.104620

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  • The nature of the Moho beneath fast‐spreading centers: Evidence from the Pacific plate and Oman ophiolite Reviewed

    Yoshihiko Tamura, Mathieu Rospabé, Gou Fujie, Akane Ohira, Kentaro Kaneda, Alexander R. L. Nichols, Georges Ceuleneer, Tomoki Sato, Shuichi Kodaira, Seiichi Miura, Eiichi Takazawa

    Island Arc   31 ( 1 )   2022.9

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    Publishing type:Research paper (scientific journal)   Publisher:Wiley  

    DOI: 10.1111/iar.12460

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    Other Link: https://onlinelibrary.wiley.com/doi/full-xml/10.1111/iar.12460

  • Titanium isotope heterogeneity in the Earth’s mantle: A case study of the Horoman peridotite massif Reviewed

    Merislava Anguelova, Manuela A. Fehr, Eiichi Takazawa, Maria Schönbächler

    Geochimica et Cosmochimica Acta   2022.7

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    Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.gca.2022.07.005

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  • The magnesium isotopic compositions of the crust and mantle: A study on the Oman ophiolite Reviewed

    Jiwon Eom, Toshihiro Yoshimura, Norikatsu Akizawa, Shigeyuki Wakaki, Tsuyoshi Ishikawa, Eiichi Takazawa, Kyoko Yamaoka, Hodaka Kawahata

    Chemical Geology   120969 - 120969   2022.6

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.chemgeo.2022.120969

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  • Petrogenesis of arc-related serpentinized peridotites (Egypt): Insights into Neoproterozoic mantle evolution beneath the Arabian-Nubian Shield Reviewed

    Mohamed Zaki Khedr, Eiichi Takazawa, Christoph Hauzenberger, Akihiro Tamura, Shoji Arai, Robert James Stern, Tomoaki Morishita, Amr El-Awady

    Journal of Asian Earth Sciences   226   105078 - 105078   2022.4

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Elsevier BV  

    DOI: 10.1016/j.jseaes.2022.105078

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  • Geochemical characterization of the Oman Crust‐Mantle transition zone, OmanDP Holes CM1A and CM2B Reviewed

    F. Kourim, M. Rospabé, N. Dygert, S. Chatterjee, E. Takazawa, K‐L. Wang, M. Godard, M. Benoit, M. Giampouras, K. Ishii, D. A‐H Teagle, M‐J. Cooper, P. Kelemen

    Journal of Geophysical Research: Solid Earth   2022.3

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    Publishing type:Research paper (scientific journal)   Publisher:American Geophysical Union (AGU)  

    DOI: 10.1029/2021jb022694

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  • Ship-board determination of whole-rock (ultra-)trace element concentrations by laser ablation-inductively coupled plasma mass spectrometry analysis of pressed powder pellets aboard the D/V Chikyu Reviewed

    Mathieu Rospabé, Fatma Kourim, Akihiro Tamura, Eiichi Takazawa, Manolis Giampouras, Sayantani Chatterjee, Keisuke Ishii, Matthew J. Cooper, Marguerite Godard, Elliot Carter, Natsue Abe, Kyaw Moe, Damon A. H. Teagle

    Scientific Drilling   30   75 - 99   2022.2

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Copernicus GmbH  

    Abstract. The Oman Drilling Project (OmanDP), performed under theInternational Continental Scientific Drilling Program (ICDP), is aninternational scientific research project that undertook drilling at a range of sites in the Semail ophiolite (Oman) to collect core samples spanning the stratigraphy of the ophiolite, from the upper oceanic crust down to the basal thrust. The cores were logged to International Ocean Discovery Program (IODP) standards aboard the D/V Chikyu. During ChikyuOman2018 Leg 3 (July–August 2018), participants described cores from the crust–mantle transition (CM) sites. The main rock types recovered at these sites weregabbros, dunites and harzburgites, rocks typically forming the base of theoceanic crust and the shallow mantle beneath present-day spreading centres.In addition to the core description, selected samples were analysed by X-ray fluorescence spectrometry (XRF) for their chemical compositions, including major, minor and some trace elements. To complement these standard procedures, we developed newapproaches to measure ultra-trace element concentrations using a procedureadapted from previous works to prepare fine-grained pressed powder pelletscoupled with laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS) analysis using instrumentation aboard the D/V Chikyu. First, three (ultra)mafic reference materials were investigated to test and validate our procedure (BHVO-2, BIR-1a and JP-1), and then the procedure was applied to a selection of gabbro and dunite samples from the CM cores toexplore the limitations of the method in its current stage of development.The obtained results are in good agreement with preferred values for thereference materials and with subsequent solution replicate analyses of the same samples performed in shore-based laboratories following Leg 3 for theCM samples. We describe this procedure for the determination of 37 minor and (ultra-)trace elements (transition elements and Ga, Li and Large-Ion Lithophile Elements (LILE), Rare Earth Elements (REE), High-Field-Strength Elements (HFSE), U, Th, and Pb) in mafic and ultramafic rocks. The presented method has the major advantage that it allows the determination at sea of the(ultra-)trace element concentrations in a “dry”, safe way, without usingacid reagents. Our new approach could be extended for other elements ofinterest and/or be improved to be adapted to other rock materials duringfuture ocean drilling operations aboard the D/V Chikyu and other platforms.

    DOI: 10.5194/sd-30-75-2022

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  • Listvenite Formation During Mass Transfer into the Leading Edge of the Mantle Wedge: Initial Results from Oman Drilling Project Hole BT1B Reviewed

    Peter B. Kelemen, Juan Carlos de Obeso, James A. Leong, Marguerite Godard, Keishi Okazaki, Alissa J. Kotowski, Craig E. Manning, Eric T. Ellison, Manuel D. Menzel, Janos L. Urai, Greg Hirth, Matthew Rioux, Daniel F. Stockli, Romain Lafay, Andreas M. Beinlich, Jude A. Coggon, Nehal H. Warsi, Jürg M. Matter, Damon A. H. Teagle, Michelle Harris, Katsuyoshi Michibayashi, Eiichi Takazawa, Zaher Al Sulaimani

    Journal of Geophysical Research: Solid Earth   127 ( 2 )   2022.2

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:American Geophysical Union (AGU)  

    DOI: 10.1029/2021jb022352

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    Other Link: https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2021JB022352

  • Deep Sourced Fluids for Peridotite Carbonation in the Shallow Mantle Wedge of a Fossil Subduction Zone: Sr and C Isotope Profiles of OmanDP Hole BT1B

    de Obeso, J.C., Kelemen, P.B., Leong, J.M., Menzel, M.D., Manning, C.E., Godard, M., Cai, Y., Bolge, L., Matter, J., Teagle, D., Coggon, J., Harris, M., Bennett, E., Bompard, N., Boulanger, M., France, L., Früh-Green, G., Garbe-Schönberg, D., Ildefonse, B., Jesus, A., Koepke, J., Koornneef, L., Lafay, R., Lissenberg, J., MacLeod, C., Mock, D., Morris, T., Müller, S., Noël, J., Nothaft, D., Perez, A., Pezard, P., Warsi, N., Zeko, D., Zihlmann, B., Bechkit, M., Brun, L., Célérier, B., Henry, G., Paris, J., Lods, G., Robert, P., Al Amri, S., Al Shukaili, M., Al Qassabi, A., Moe, K., Yamada, Y., Takazawa, E., Michibayashi, K., Abe, N., Akitou, T., AlShahri, S.A., Hamed Shames Al-Siyabi, H., Alhumaimi, S.M., AlRawahi, M.H., Al Sarmi, M.S., Alwaeli, B.H., Beinlich, A., Carter, E., Cheadle, M., Cloos, M., Cooper, M., Crispini, L., Deamer, L., Deans, J., Faak, K., Greenberger, R., Harigane, Y., Hatakeyama, K., Horst, A., Hoshide, T., Ishii, K., Johnson, K., Kettermann, M., Kim, H., Kondo, K., Kotowski, A., Kourim, F., Kusano, Y., Menzies, C., Morishita, T., Nguyen, D.K., Nozaka, T., Okazaki, K., Picazo, S., Senda, R., Tateishi, Y., Till, J., Umino, S., Urai, J., Usui, Y., D’Andres, J.

    Journal of Geophysical Research: Solid Earth   127 ( 1 )   2022

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    Publishing type:Research paper (scientific journal)  

    DOI: 10.1029/2021JB022704

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  • Initial Results From the Oman Drilling Project Multi‐Borehole Observatory: Petrogenesis and Ongoing Alteration of Mantle Peridotite in the Weathering Horizon Reviewed

    Peter B. Kelemen, James A. Leong, Juan Carlos de Obeso, Jürg M. Matter, Eric T. Ellison, Alexis Templeton, Daniel B. Nothaft, Alireza Eslami, Katy Evans, Marguerite Godard, Benjamin Malvoisin, Jude A. Coggon, Nehal H. Warsi, Philippe Pézard, Saebyul Choe, Damon A. H. Teagle, Katsuyoshi Michibayashi, Eiichi Takazawa, Zaher Al Sulaimani

    Journal of Geophysical Research: Solid Earth   126 ( 12 )   2021.12

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:American Geophysical Union (AGU)  

    DOI: 10.1029/2021jb022729

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    Other Link: https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2021JB022729

  • Operating outdated EPMA (JXA-8600SX) by popular microcomputers and Windows PC Reviewed

    Hayato Ueda, Eiichi Takazawa

    The Journal of the Geological Society of Japan   127 ( 11 )   681 - 686   2021.11

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    Language:Japanese   Publishing type:Research paper (scientific journal)   Publisher:The Geological Society of Japan  

    DOI: 10.5575/geosoc.2021.0028

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  • Achievements and Future Prospects of the ICDP Oman Drilling Project Invited Reviewed

    Eiichi TAKAZAWA

    Journal of Geography (Chigaku Zasshi)   130 ( 4 )   507 - 525   2021.8

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    Authorship:Lead author, Corresponding author   Language:Japanese   Publishing type:Research paper (scientific journal)   Publisher:Tokyo Geographical Society  

    DOI: 10.5026/jgeography.130.507

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  • Orthopyroxene–magnetite symplectite in olivine gabbros from the lower crustal Oman Ophiolite: Oman Drilling Project, Hole GT2A Reviewed

    Sayantani CHATTERJEE, Debaditya BANDYOPADHYAY, Eiichi TAKAZAWA, Katsuyoshi MICHIBAYASHI

    Journal of Mineralogical and Petrological Sciences   116 ( 3 )   170 - 175   2021.6

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Japan Association of Mineralogical Sciences  

    DOI: 10.2465/jmps.201130f

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  • Trace and rare earth element geochemistry of clinopyroxene in mafic dykes from Western Dharwar craton, southern India

    Sasidharan A. SILPA, M. SATISH–KUMAR, Eiichi TAKAZAWA, Krishnan SAJEEV

    Journal of Mineralogical and Petrological Sciences   116 ( 2 )   108 - 112   2021

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    Publishing type:Research paper (scientific journal)   Publisher:Japan Association of Mineralogical Sciences  

    DOI: 10.2465/jmps.201130c

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  • High resolution X–ray computed tomography and scanning electron microscopy studies of multiphase solid inclusions in Oman podiform chromitite: implications for post–entrapment modification Reviewed

    Yuan YAO, Eiichi TAKAZAWA, Sayantani CHATTERJEE, Antonin RICHARD, Christophe MORLOT, Laura CR{\'{E } }ON, Salim AL{\textendash}BUSAIDI, Katsuyoshi MICHIBAYASHI

    Journal of Mineralogical and Petrological Sciences   115 ( 3 )   247 - 260   2020.4

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Japan Association of Mineralogical Sciences  

    DOI: 10.2465/jmps.191008

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  • The non-chondritic Ni isotope composition of Earth's mantle Reviewed

    Martijn Klaver, Dmitri A. Ionov, Eiichi Takazawa, Tim Elliott

    GEOCHIMICA ET COSMOCHIMICA ACTA   268   405 - 421   2020.1

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    Language:English   Publishing type:Research paper (scientific journal)  

    DOI: 10.1016/j.gca.2019.10.017

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  • Scientific Drilling Across the Shoreline Reviewed

    Sean Gulick, Kenneth Miller, Peter Keleman, Joanna Morgan, Jean-Noel Proust, Eiichi Takazawa

    Oceanography   32 ( 1 )   157 - 159   2019.3

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:The Oceanography Society  

    DOI: 10.5670/oceanog.2019.139

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  • In situ carbon mineralization in ultramafic rocks: Natural processes and possible engineered methods Reviewed

    P.B. Kelemen, R. Aines, E. Bennett, S.M. Benson, E. Carter, J.A. Coggon, J.C. de Obeso, O. Evans, G. Gadikota, G.M. Dipple, M. Godard, M. Harris, J.A. Higgins, K.T.M. Johnson, F. Kourim, R. Lafay, S. Lambart, C.E. Manning, J.M. Matter, K. Michibayashi, T. Morishita, J. Noël, K. Okazaki, P. Renforth, B. Robinson, H. Savage, R. Skarbek, M.W. Spiegelman, E. Takazawa, D. Teagle, J.L. Urai, J. Wilcox

    Energy Procedia   146   92 - 102   2018.7

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:Elsevier {BV}  

    DOI: 10.1016/j.egypro.2018.07.013

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  • Tectonic affinities of the accreted basalts in southern Taiwan Reviewed

    Hsin-Yu Chen, Huai-Jen Yang, Yung-Hsin Liu, Kuo-Fang Huang, Eiichi Takazawa

    JOURNAL OF ASIAN EARTH SCIENCES   158   253 - 265   2018.6

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    DOI: 10.1016/j.jseaes.2018.02.015

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  • Evaluation of time-resolved mean-of-ratios reduction for laser ablation zircon U-Pb dating using quadrupole ICPMS Reviewed

    Hayato Ueda, Eiichi Takazawa, Rinpei Kato, Yoshiko Adachi

    GEOCHEMICAL JOURNAL   52 ( 3 )   241 - 254   2018

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    DOI: 10.2343/geochemj.2.0509

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  • Reductive Heating Experiments on BOF-Slag: Simultaneous Phosphorus Re-Distribution and Volume Stabilization for Recycling Reviewed

    Tung-Hsin Su, Huai-Jen Yang, Yu-Chen Lee, Yen-Hong Shau, Eiichi Takazawa, Ming-Fong Lin, Jin-Luh Mou, Wei-Teh Jiang

    STEEL RESEARCH INTERNATIONAL   87 ( 11 )   1511 - 1526   2016.11

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    DOI: 10.1002/srin.201500441

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  • Distribution and hosts of arsenic in a sediment core from the Chianan Plain in SW Taiwan: Implications on arsenic primary source and release mechanisms Reviewed

    Huai-Jen Yang, Chi-Yu Lee, Yu-Ju Chiang, Jiin-Shuh Jean, Yen-Hong Shau, Eiichi Takazawa, Wei-Teh Jiang

    SCIENCE OF THE TOTAL ENVIRONMENT   569   212 - 222   2016.11

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    DOI: 10.1016/j.scitotenv.2016.06.122

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  • Sr and Nd Isotopic evidence in metacarbonate rocks for an extinct Island arc-ocean system in East Antarctica Reviewed

    Naho Otsuji, M. Satish-Kumar, Atsushi Kamei, Eiichi Takazawa, Noriyoshi Tsuchiya, G. H. Grantham, Tetsuo Kawakami, Masahiro Ishikawa, Yasuhito Osanai

    JOURNAL OF MINERALOGICAL AND PETROLOGICAL SCIENCES   111 ( 3 )   170 - 180   2016.6

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    DOI: 10.2465/jmps.151029a

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  • CO2 sequestration utilizing basic-oxygen furnace slag: Controlling factors, reaction mechanisms and V-Cr concerns Reviewed

    Tung-Hsin Su, Huai-Jen Yang, Yen-Hong Shau, Eiichi Takazawa, Yu-Chen Lee

    JOURNAL OF ENVIRONMENTAL SCIENCES   41   99 - 111   2016.3

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    DOI: 10.1016/j.jes.2015.06.012

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  • Across-arc variations in geochemistry of Oligocene to Quaternary basalts from the NE Japan arc: Constraints on source composition, mantle melting and slab input composition Reviewed

    Shuto, K., Nohara-Imanaka, R., Sato, M., Takahashi, T., Takazawa, E., Kawabata, H., Takanashi, K., Ban, M., Watanabe, N., Fujibayashi, N.

    Journal of Petrology   56 ( 11 )   2257 - 2294   2015.12

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    DOI: 10.1093/petrology/egv073

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  • Decoupling of the Lu-Hf, Sm-Nd, and Rb-Sr isotope systems in eclogites and a garnetite from the Sulu ultra-high pressure metamorphic terrane: Causes and implications Reviewed

    Yung-Hsin Liu, Huai-Jen Yang, Eiichi Takazawa, Madhusoodhan Satish-Kumar, Chen-Feng You

    LITHOS   234   1 - 14   2015.10

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    DOI: 10.1016/j.lithos.2015.07.013

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  • The influence of melt infiltration on the Li and Mg isotopic composition of the Horoman Peridotite Massif Reviewed

    Yi-Jen Lai, Philip A. E. Pogge von Strandmann, Ralf Dohmen, Eiichi Takazawa, Tim Elliott

    GEOCHIMICA ET COSMOCHIMICA ACTA   164   318 - 332   2015.9

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    DOI: 10.1016/j.gca.2015.05.006

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  • Compositional and Sr-Nd-Hf isotopic variations of Baijingsi eclogites from the North Qilian orogen, China: Causes, protolith origins, and tectonic implications Reviewed

    Choon-Muar Ker, Huai-Jen Yang, Jianxin Zhang, Yen-Hong Shau, Chia-Ju Chieh, Fancong Meng, Eiichi Takazawa, Chen-Feng You

    GONDWANA RESEARCH   28 ( 2 )   721 - 734   2015.9

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    DOI: 10.1016/j.gr.2014.06.006

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  • Melt extraction and metasomatism recorded in basal peridotites above the metamorphic sole of the northern Fizh massif, Oman ophiolite Reviewed

    Masako Yoshikawa, Marie Python, Akihiro Tamura, Shoji Arai, Eiichi Takazawa, Tomoyuki Shibata, Akira Ueda, Tsutomu Sato

    TECTONOPHYSICS   650   53 - 64   2015.5

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    DOI: 10.1016/j.tecto.2014.12.004

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  • Repeated magmatism at 34 Ma and 23-20 Ma producing high magnesian adakitic andesites and transitional basalts on southern Okushiri Island, NE Japan arc Reviewed

    Makoto Sato, Kenji Shuto, Rikako Nohara-Imanaka, Eiichi Takazawa, Yasuhito Osanai, Nobuhiko Nakano

    LITHOS   205   60 - 83   2014.9

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    DOI: 10.1016/j.lithos.2014.06.008

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  • A kilometre-scale highly refractory harzburgite zone in the mantle section of the northern oman ophiolite (fizh block): Implications for flux melting of oceanic lithospheric mantle Reviewed

    Nami Kanke, Eiichi Takazawa

    Geological Society Special Publication   392 ( 1 )   229 - 246   2014

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    DOI: 10.1144/SP392.12

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  • Petrological nature and origin of the ultramafic complex in the basal part of the Salahi mantle section, the Oman ophiolite Reviewed

    野本有希, 高澤栄一

    岩石鉱物科学   42 ( 3 )   123-135 (J-STAGE) - 135   2013

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    Extensive lenticular-shaped ultramafic complexes that are composed of dominant amount of dunite associated with harzburgite and irregular-shaped pyroxenite cumulates, occur in the basal part of the Salahi mantle section in the northern Oman ophiolite. Petrologic characteristics such as rock types, textures and mineral compositions were examined to understand the origin of the ultramafic complex. Peridotites exhibit coarse-granular to very coarse-granular texture with grain size greater than five millimeters. The Cr#[=Cr/(Cr+Al) atomic ratio] of spinels in harzburgites ranges from 0.56 to 0.72, and is most frequent at 0.64-0.66 while spinel Cr# of dunites ranges from 0.61 to 0.84, and is most frequent at 0.76-0.82. The origin of voluminous dunite with high Cr# spinel can be explained by flux melting of residual harzburgite as a result of infiltration of large amount of fluid from the base of the ophiolite during oceanic thrusting. Dunites with very coarse-granular texture also support this hypothesis. The dunites in the central part of the complex tend to have both olivine Fo content and spinel Cr# greater than those in the host harzburgites. We speculate that not only orthopyroxene but also olivine were consumed during flux melting in this region resulted in the formation of voluminous dunites in the core of the complex. On the other hand, the dunites from the periphery of the complex have olivine with Fo content lower than those in the host harzburgites indicating precipitation of olivine from the melt. Moreover, crystallization of pyroxene formed numerous pyroxenites in this region. The southern part of the Salahi mantle section has been considered as a paleo-ridge segment end region. Our results support that the occurrence of highly refractory peridotites is spatially related to the segment end region in the northern Oman ophiolite.<br>

    DOI: 10.2465/gkk.120624

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  • Scientific drilling and related research in the samail ophiolite, sultanate of Oman Reviewed

    Peter Kelemen, Ali Al Rajhi, Marguerite Godard, Benoit Ildefonse, Jürgen Köpke, Chris MacLeod, Craig Manning, Katsu Michibayashi, Sobhi Nasir, Everett Shock, Eiichi Takazawa, Damon Teagle

    Scientific Drilling   ( 15 )   64 - 71   2013

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    DOI: 10.2204/iodp.sd.15.10.2013

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  • スコットランド南東部シッカー岬とハットンの不整合 Reviewed

    道林克禎, 森下知晃, 村山雅史, 西弘嗣, 尾鼻浩一郎, 鈴木庸平, 高澤栄一, 山田泰広, 横山祐典

    地質学雑誌   118 ( 11 )   IX-X - X   2012.11

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    DOI: 10.5575/geosoc.118.11.IX_X

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  • Preface Reviewed

    MORISHITA Tomoaki, ABE Natsue, MIZUKAMI Tomoyuki, OZAWA Kazuhito, TAKAZAWA Eiichi

    Japanese Magazine of Mineralogical and Petrological Sciences   41 ( 5 )   171 - 173   2012.9

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    &amp;nbsp;&amp;nbsp;How much do we know the Earth&#039;s mantle? We would like to make clear what we want to know, what we can know and what we will be able to know the Earth&#039;s mantle. This special issue focuses on recent scientific advances in serpentinization, pressure-temperature paths including thermal history of the earth, tectono-magmatic processes, geochemical recycling, rheology and chemical compositions of the Earth&#039;s mantle based on analyses of mantle-derived materials including volcanic rocks. These topics provide useful information for a wide range of earth scientific communities.&lt;br&gt;

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  • Melting and reaction in an incipient subarc mantle as inferred from the spatial compositional variability in the mantle section of the Oman ophiolite Reviewed

    Eiichi Takazawa

    Japanese Magazine of Mineralogical and Petrological Sciences   41 ( 6 )   257 - 266   2012

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    DOI: 10.2465/gkk.120704

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  • The mohole: A crustal journey and mantle quest, workshop in Kanazawa, Japan, 3-5 June 2010 Reviewed

    Benoît Ildefonse, Natsue Abe, Donna K. Blackman, J. Pablo Canales, Yoshio Isozaki, Shuichi Kodaira, Greg Myers, Kentaro Nakamura, Mladen Nedimovic, Alexander C. Skinner, Nobukazu Seama, Eiichi Takazawa, Damon A.H. Teagle, Masako Tominaga, Susumu Umino, Douglas S. Wilson, Masaoki Yamao

    Scientific Drilling   10, 56-63 ( 10 )   56 - 63   2010.9

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    DOI: 10.2204/iodp.sd.10.07.2010

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  • Shallow Mantle Composition and Dynamics: Fifth International Orogenic Lherzolite Conference Reviewed

    Martin Menzies, Peter Kelemen, Henry Dick, Jean-Louis Bodinier, Francoise Boudier, Greg Hirth, Tim Grove, Andrea Tommasi, Eiichi Takazawa

    JOURNAL OF PETROLOGY   51 ( 1-2 )   3 - 7   2010.1

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  • Primary melting sequence of a deep (&gt; 250 km) lithospheric mantle as recorded in the geochemistry of kimberlite-carbonatite assemblages, Snap Lake dyke system, Canada Reviewed

    A. M. Agashev, N. P. Pokhilenko, E. Takazawa, J. A. McDonald, M. A. Vavilov, T. Watanabe, N. V. Sobolev

    Chemical Geology   255 ( 3-4 )   317 - 328   2008.10

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    DOI: 10.1016/j.chemgeo.2008.07.003

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  • Origin of layering observed in the Horoman peridotite complex, Japan

    Niida Kiyoaki, Takasawa Eiichi

    The Journal of the Geological Society of Japan   113   S167 - S184   2007

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    DOI: 10.5575/geosoc.113.S167

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  • Corundum-bearing mafic granulites in the Horoman (Japan) and Ronda (Spain) peridotite massifs: Possible remnants of recycled crustal materials in the mantle Reviewed

    Morishita, T., Takazawa, E., Arai, S., Obata, M., Kodera, T., Gervilla, F.

    Island Arc   15 ( 1 )   2 - 3   2006.3

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    DOI: 10.1111/j.1440-1738.2006.00517.x

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  • Geochemical secular variation of magma source during Early to Middle Miocene time in the Niigata area, NE Japan: Asthenospheric mantle upwelling during back-arc basin opening Reviewed

    K Shuto, H Ishimoto, Y Hirahara, M Sato, K Matsui, N Fujibayashi, E Takazawa, K Yabuki, M Sekine, M Kato, AI Rezanov

    LITHOS   86 ( 1-2 )   1 - 33   2006.1

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    DOI: 10.1016/j.lithos.2005.06.001

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  • Compositional continuity and discontinuity in the Horoman peridotite, Japan, and its implication for melt extraction processes in partially molten upper mantle Reviewed

    M Obata, E Takazawa

    JOURNAL OF PETROLOGY   45 ( 2 )   223 - 234   2004.2

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  • P-211 Hybridization of dunite and gabbroic materials observed in Hole 1271B, ODP Leg 209

    Takazawa Eiichi, Abe Natsue, Kikawa Eiichi

    Annual Meeting of the Geological Society of Japan   2004   265 - 265   2004

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    DOI: 10.14863/geosocabst.2004.abst.0_265_1

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  • Geochemistry and origin of the basal lherzolites from the northern Oman ophiolite (northern Fizh block) Reviewed

    E Takazawa, T Okayasu, K Satoh

    GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS   4   2003.2

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    DOI: 10.1029/2001GC000232

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  • Model of layering formation in a mantle peridotite (Horoman,Hokkaido, Japan) Reviewed

    Toramaru, A., Takazawa, E., Morishita, T., Matsukage, K.

    Earth and Planetary Science Letters   185 ( 3-4 )   299 - 313   2001.3

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    DOI: 10.1016/S0012-821X(00)00382-4

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  • Re-Os isotopes in the Horoman peridotite: Evidence for refertilization? Reviewed

    AE Saal, E Takazawa, FA Frey, N Shimizu, Hart, SR

    JOURNAL OF PETROLOGY   42 ( 1 )   25 - 37   2001.1

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  • Whole rock compositional variations in an upper mantle peridotite (Horoman, Hokkaido, Japan): Are they consistent with a partial melting process? Reviewed

    E Takazawa, FA Frey, N Shimizu, M Obata

    GEOCHIMICA ET COSMOCHIMICA ACTA   64 ( 4 )   695 - 716   2000.2

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  • Permian brachiopods from the Okutadami area, near the boundary between Niigata and Fukushima Prefectures, central Japan and their tectonic implications Reviewed

    Tazawa Jun-ichi, Ando Susumu, Furuhashi Shinya, Furuta Kozue, Okayasu Toshie, Shimura Toshiaki, Takazawa Eiichi, Tateishi Masaaki, Watanabe Satoshi, Yamamoto Kazumi, Yamamoto Ryo, Toyoshima Tsuyoshi, Okochi Makoto

    Journal of the Geological Society of Japan   105 ( 10 )   729 - 732   1999.10

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    The following four brachiopod species are newly recognized from the Okutadami area, central Japan : Anemonaria sp., Yokovlevia sp., Spiriferella sp. and Attenuatella sp. These brachiopods indicate a late Middle Permian (Midian) in age. The Okutadami fauna, consisting of both the Boreal- and Bipolar-type genera, is the first documented Permian Boreal brachiopod fauna in Japan. The occurrence of the Boreal brachiopod fauna from the Okutadami area suggests that the fossil-bearing rocks were formed at the northernmost part of Japan in the Permian time.

    DOI: 10.5575/geosoc.105.729

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  • Non-chondritic platinum-group element ratios in oceanic mantle lithosphere: petrogenetic signature of melt percolation? Reviewed

    M Rehkamper, AN Halliday, J Alt, JG Fitton, J Zipfel, E Takazawa

    EARTH AND PLANETARY SCIENCE LETTERS   172 ( 1-2 )   65 - 81   1999.10

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  • Polybaric petrogenesis of mafic layers in the Horoman peridotite complex, Japan Reviewed

    E. Takazawa, F. A. Frey, N. Shimizu, A. Saal, M. Obata

    Journal of Petrology   40 ( 12 )   1827 - 1851   1999

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    DOI: 10.1093/petroj/40.12.1827

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  • Petrogenesis of mafic layers in the Horoman peridotite complex, Japan

    Takazawa, E., Frey, F.A., Shimizu, N., Saal, A., Obata, M.

    Ofioliti   24 ( 1 A )   173 - 173   1999

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  • Abundances of trace elements in clinopyroxenes from the Horoman peridotite complex: Evidence of reaction with exotic melt/fluid

    Takazawa, E., Frey, F.A., Shimizu, N.

    Ofioliti   24 ( 1 A )   1999

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  • Re-Os isotopic composition of Horoman peridotite: Implications for the genesis of the plagioclase-lherzolite and the layered structure

    Saal, A., Takazawa, E., Frey, F.A., Shimizu, N., Hart, S.

    Ofioliti   24 ( 1 A )   160 - 160   1999

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  • Collapsing carbon nanotubes and diamond formation under shock waves Reviewed

    Y. Q. Zhu, T. Sekine, T. Kobayashi, E. Takazawa, M. Terrones, H. Terrones

    Chemical Physics Letters   287 ( 5-6 )   689 - 693   1998.5

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    DOI: 10.1016/S0009-2614(98)00226-7

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  • Radiation temperatures of soda-lime glass in its shock-compressed liquid state Reviewed

    T. Kobayashi, T. Sekine, O. V. Fat'yanov, E. Takazawa, Q. Y. Zhu

    Journal of Applied Physics   83 ( 3 )   1711 - 1716   1998.2

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    Language:English   Publishing type:Research paper (scientific journal)   Publisher:American Institute of Physics Inc.  

    DOI: 10.1063/1.366889

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  • Shock-induced phase transitions among SiC polytypes Reviewed

    Y. Q. Zhu, T. Sekine, T. Kobayashi, E. Takazawa

    Journal of Materials Science   33 ( 24 )   5883 - 5890   1998

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    DOI: 10.1023/A:1004482922441

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  • Hugoniot equation of state and high-pressure transformation of jadeite

    Takazawa, E., Sekine, T., Kobayashi, T., Zhu, Y.

    Journal of Geophysical Research: Solid Earth   103 ( 6 )   1998

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  • High pressure carbon behavior induced from carbide Hugoniots

    T. Sekine, E. Takazawa, T. Kobayashi

    Materials Research Society Symposium - Proceedings   499   99 - 104   1998

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  • Evolution of the Horoman Peridotite (Hokkaido, Japan): Implications from pyroxene compositions Reviewed

    E Takazawa, F Frey, N Shimizu, M Obata

    CHEMICAL GEOLOGY   134 ( 1-3 )   3 - 26   1996.12

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  • Magma transport and metasomatism in the mantle: A critical review of current geochemical models - Discussion

    Navon, O., Frey, F.A., Takazawa, E.

    American Mineralogist   81 ( 5-6 )   1996

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    DOI: 10.2138/am-1996-5-622

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  • GEOCHEMICAL EVIDENCE FOR MELT MIGRATION AND REACTION IN THE UPPER MANTLE Reviewed

    E TAKAZAWA, FA FREY, N SHIMIZU, M OBATA, JL BODINIER

    NATURE   359 ( 6390 )   55 - 58   1992.9

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  • Compositional Variations within the Lower Layered Zone of the Horoman Peridotite, Hokkaido, Japan: Constraints on Models for Melt-Solid Segregation Reviewed

    Fred A. Frey, N. Shimizu, A. Leinbach, M. Obata, E. Takazawa

    JOURNAL OF PETROLOGY   211 - 227   1991

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  • Manganese nodules from the Upper Cretaceous Yubetsu Group, eastern Hokkaido, Japan Reviewed

    Masayuki SAKAKIBARA, Kiyoaki NIIDA, Kenji TOGARI, Masahide AKASAKA, Eiichi TAKASAWA, Yoshihiko GOTO, Masako YOSHIKAWA, Gaku KIMURA, Norio KITO, Jun TAJIKA, Takayuki KATO, Hideaki TODA

    Jour. Geol. Soc. Japan.   95 ( 3 )   241 - 244   1989

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    DOI: 10.5575/geosoc.95.241

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  • マフィック岩を包有する不均質なマントルの部分融解に関する地質学的検証

    高澤, 栄一

    [高澤栄一]  2006 

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MISC

  • Oman Drilling Project Phase1のリストヴェナイト中のドロマイト脈に薄い塩水からなる流体包有物があるぜよ

    川本竜彦, 佐藤宏樹, 高橋藤馬, GUOTANA Juan Miguel, 森下知晃, KELEMEN Peter B, COGGON Jude Ann, HARRIS Michelle, MATTER Juerg Michael, 道林克禎, 高澤栄一, TEAGLE Damon A H

    日本地球惑星科学連合大会予稿集(Web)   2019   2019

  • オマーンオフィオライトWadi Tayin岩体における地殻-マントル境界の岩石学および地球化学的特徴

    高澤栄一, 高澤栄一, 木暮優芽斗, CHATTERJEE Sayantani, 小柳夏希, 道林克禎, 田村芳彦

    日本地質学会学術大会講演要旨   126th   2019

  • Mantle-melt interaction at the crust-mantle boundary in the Wadi Tayin massif, the Oman mantle peridotite

    高澤栄一, 高澤栄一, 木暮優芽斗, 石井慶佑, CHATTERJEE Sayantani, 小柳夏希, 道林克禎, 田村芳彦

    日本鉱物科学会年会講演要旨(Web)   2019   2019

  • モホのつくり方

    田村芳彦, 高澤栄一, 高澤栄一, CEULENEER Georges, 道林克禎, 佐藤智紀, 小平秀一, 三浦誠一

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

  • オマーン陸上掘削第1期ChikyuOman2017におけるオフィオライト地殻セクションの岩石物性研究速報

    阿部なつ江, 岡崎啓史, 畠山航平, ILDEFONSE Benoit, LEONG James Andrew, 立石大和, 道林克禎, 高澤栄一, KELEMEN Peter, TEAGLE Damon A H, HARRIS Michelle, COGGON Jude Ann, DE OBESO Juan Calros, MATTER Juerg

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

  • オマーン陸上掘削第1期ChikyuOman2017における岩石物性研究速報

    阿部なつ江, 岡崎啓史, 畠山航平, ILDEFONSE Benoit, 立石大和, LEONG James Andrew, 道林克禎, 高澤栄一, KELEMEN Peter, TEAGLE Damon, HARRIS Michelle

    ブルーアースサイエンス・テク要旨集   2018   2018

  • モホ反射面のつくりかた

    田村芳彦, 藤江剛, 大平茜, 高澤栄一, CEULENEER Georges, 道林克禎, 佐藤智紀, 小平秀一, 三浦誠一

    日本地質学会学術大会講演要旨   125th   2018

  • Physical property measurement of ICDP Oman Drilling Project (ChikyuOman2017) Phase I-From Oceanic Plate to obduction stage

    阿部なつ江, 岡崎啓史, 畠山航平, ILDEFONSE Benoit, 立石大和, LEONG James Andrew, 道林克禎, 高澤栄一, KELEMEN Peter, DE OBESO Juan Calros, TEAGLE Damon, COGGON Jude, HARRIS Michelle

    日本鉱物科学会年会講演要旨(Web)   2018   2018

  • オマーンオフィオライト南部でのハンレイ岩-カンラン岩関係

    森下知晃, 荒井章司, KELEMEN Peter, TEAGLE Damon, 石井慶佑, 高澤栄一, NGUYEN Khac Du, COGGON Jude, MATTER Juerg, 道林克禎, 田村芳彦, MOE KhawThu, 山田泰広

    日本地質学会学術大会講演要旨   125th   2018

  • オマーン掘削プロジェクト速報:海洋プレート層序のXCTプロファイル

    道林克禎, 高澤栄一, KELEMEN Peter, TEAGLE Damon, HARRIS Michelle, GODARD Marguerite

    日本地質学会学術大会講演要旨   125th   2018

  • ICDPオマーン陸上掘削コア試料に記録されているモホ遷移帯の岩石物性について

    阿部なつ江, MOE Kyaw, 山田泰広, 岡崎啓史, 畠山航平, 赤松祐哉, 片山郁夫, 高澤栄一, 道林克禎, KELEMEN Peter, TEAGLE Damon

    日本地質学会学術大会講演要旨   125th   2018

  • ICDP Oman Drilling Project:オマーンオフィオライトWadi Tayin岩体における地殻-マントル境界の掘削

    高澤栄一, COGGON Jude, KELEMEN Peter, MATTER Juerg, 道林克禎, 森下知晃, 田村芳彦, TEAGLE Damon, KHAW Thu Moe, 山田泰広

    日本地質学会学術大会講演要旨   125th   2018

  • 国際陸上掘削計画による沈み込むプレート境界相当岩石コア(オマーンオフィオライト基底部Listvenite/変成岩境界)の海洋掘削船CHIKYUを用いた記載とその成果

    森下知晃, KELEMEN B. Peter, COGGON Judith, MATTER Juerg, HARRIS Michelle, 道林克禎, 高澤栄一, TEAGLE A.H. Damon, GODARD Marguerite

    日本鉱物科学会年会講演要旨(Web)   2018   2018

  • オマーンオフィオライト・ワディタイン岩体CMサイトにおける地殻-マントル遷移帯の陸上掘削

    高澤栄一, COGGON Jude Ann, KELEMEN Peter B, MATTER Juerg Michael, 道林克禎, 田村芳彦, TEAGLE Damon A H, KHAWTHU Moe, 山田泰広

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

  • マントルウエッジプレート境界掘削:オマーン陸上掘削-サマイル・オフィオライトの炭酸塩岩化したカンラン岩から下位の変成岩までの掘削成果概要

    森下知晃, KELEMEN Peter B, COGGON Judith, MATTER Juerg, HARRIS Michelle, 道林克禎, 高澤栄一, TEAGLE Damon A H, GODARD Marguerti

    日本地球惑星科学連合大会予稿集(Web)   2018   2018

  • 海洋底下部地殻ハンレイ岩相の白金族元素存在度とOs同位体組成:ICDP Oman Drilling Project phase1速報

    仙田量子, 鈴木勝彦, 森下知晃, KELEMEN Peter, TEAGLE Damon, 高澤栄一, COGGON Jude, MATTER M. Juerg, HARRIS Michelle, 道林克禎

    日本地球化学会年会要旨集(Web)   65th   2018

  • マントル掘削計画~海と陸とちきゅうと~

    道林克禎, 高澤栄一, 田村芳彦, 小原泰彦, 岡本敦, 森下知晃, 石塚治, 針金由美子, 藤江剛, 片山郁夫, 渡邊了

    ブルーアース要旨集   2017   2017

  • Report of the 2nd International Symposium on Earth History of Asia, 31 October – 3 November, 2014, Niigata, Japan

    Science reports of Niigata University. (Geology)   30   89 - 96   2015.3

  • Protolith of metamorphic sole in the Oman ophiolite inferred from whole rock trace element abundances and Sr-Nd isotope ratios

    Takazawa Eiichi, Mori Namiko, Nohara Rikako, Takahashi Toshiro, Adachi Yoshiko, Miyashita Sumio

    Science reports of Niigata University. (Geology)   29   48 - 49   2014.10

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  • モホ点描―超深部掘削で何がわかるのか?オマーンオフィオライト・サラヒ岩体マントルセクションの鉱物組成分布からみた海嶺‐島弧変遷プロセス

    高澤栄一, 春日良一, 山野井陽一

    月刊地球   34 ( 4 )   252 - 257   2012.4

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  • モホ点描―超深部掘削で何がわかるのか?オマーンオフィオライト・フィズ岩体のマントルセクションに分布するダナイトの空間的な組成変動と成因について

    末武杏奈, 高澤栄一

    月刊地球   34 ( 4 )   247 - 251   2012.4

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  • The MoHole: A Crustal Journey and Mantle Quest Workshop Report

    ILDEFONSE Benoît, ABE Natsue, BLACKMAN Donna K, CANALES J. Pablo, ISOZAKI Yoshio, KODAIRA Shuichi, MYERS Greg, NAKAMURA Kentaro, NEDIMOVIC Mladen, SKINNER Alesander, SEAMA Nobukazu, TAKAZAWA Eiichi, TEAGLE Damon A.H, TOMINAGA Masako, UMINO Susumu, WILSON Douglas S, YAMAO Masaoki

    Workshop Report   1-67   2010.6

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  • Ridge segmentation and compositional variation in the mantle section of the Fizh Block, the Oman ophiolite

    Chikyu monthly   30 ( 2 )   86 - 93   2008.4

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  • Hybridization of dunite and gabbroic materials in Hole 1271B from Mid-Atlantic Ridge 15°N : Implications for melt flow and reaction in the upper mantle

    TAKAZAWA E.

    Proceedings of the Ocean Drilling Program. Scientific Reports, College Station, TX (Ocean Drilling Program), 2007   209   1 - 23   2007

  • Spatial variation of trace element abundances in clinopyroxenes from the layered orogenic lherzolite (Horoman peridotite, Japan): Implications for melt flow and reaction in the upper mantle

    E Takazawa, FA Frey, N Shimizu, M Obata, JL Bodinier

    GEOCHIMICA ET COSMOCHIMICA ACTA   67 ( 18 )   A471 - A471   2003.9

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    Language:English   Publishing type:Research paper, summary (international conference)  

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  • マントル内の延性せん断帯の空間分布から読みとる海洋プレートの断片化過程 北部オマーンオフィオライトの例

    道林克禎, 高沢栄一, 岡安冬恵

    日本地質学会学術大会講演要旨   108th   2001

  • Whole-rock compositional variations in an upper mantle peridotite (Horoman, Hokkaido, Japan) : implications for melt segregation, migration and reaction.

    TAKAZAWA E.

    Geochim. Cosmosim. Act.   64   717 - 732   2000

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Presentations

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Awards

  • Paper Award

    2021.9   Japan Association of Mineralogical Sciences   Yao, Y., Takazawa, E., Chatterjee, S., Richard, A., Morlot, C., Créon, L., Al–Busaidi, S., Michibayashi, K., Oman Drilling Project Science Team (2020) High resolution X–ray computed tomography and scanning electron microscopy studies of multiphase solid inclusions in Oman podiform chromitite: implications for post–entrapment modification. Journal of Mineralogical and Petrological Sciences, 115, 247–260.

    Eiichi Takazawa, Katsuyoshi Michibayashi

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Research Projects

  • Clarification of alteration of the upper mantle in the mid-ocean ridge and subduction zone

    Grant number:20H02005

    2020.4 - 2025.3

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)

    Research category:Grant-in-Aid for Scientific Research (B)

    Awarding organization:Japan Society for the Promotion of Science

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    Authorship:Principal investigator 

    Grant amount:\17550000 ( Direct Cost: \13500000 、 Indirect Cost:\4050000 )

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  • Physical properties of uppermost mantle structure and the Mohorovicic seismic discontinuity

    Grant number:16H06347

    2016.5 - 2021.3

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (S)

    Research category:Grant-in-Aid for Scientific Research (S)

    Awarding organization:Japan Society for the Promotion of Science

    Michibayashi Katsuyoshi

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    Grant amount:\184210000 ( Direct Cost: \141700000 、 Indirect Cost:\42510000 )

    In order to clarify the structure of the uppermost mantle and the formation process of the Mohorovicic discontinuity (Moho), which is the crust-mantle boundary, this study was carried out using a multifaceted approach, including microstructural analysis, measurements of physical properties, and rock-water reaction experiments, mainly on marine and terrestrial peridotites. We confirmed that the microstructure of peridotite at depths of 6,000 m or more in the Ogasawara Trench has been affected by water, and elucidated the new dynamics of deep fluids involved in rock-water reactions. We drilled the Oman ophiolite body in the Arabian Peninsula and successfully recovered continuous samples of crustal to mantle materials, and their analyses provided numerous insights for quantitative understanding of rock-fluid reaction processes in oceanic plates. Based on these results, we have developed a new model for the formation of the Moho surface and a model for the uppermost mantle structure.

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  • Elucidations of the physical properties and actual condition of the crust-mantle boundary (Moho) by onshore drilling of the Oman Ophiolite

    Grant number:16H02742

    2016.4 - 2020.3

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (A)

    Research category:Grant-in-Aid for Scientific Research (A)

    Awarding organization:Japan Society for the Promotion of Science

    TAKAZAWA Eiichi

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    Authorship:Principal investigator  Grant type:Competitive

    Grant amount:\45110000 ( Direct Cost: \34700000 、 Indirect Cost:\10410000 )

    We participated in the International Continental Scientific Drilling Program (ICDP) Oman drilling project and carried out onshore drilling of the crust-mantle boundary in the Oman ophiolite. In the Holes CM1A and CM2B of Wadi Tayin massif, we succeeded in completely collecting the drilling core with a recovery rate of 100%. As a result of drilling, it was revealed that there is a 150m thick lithology mainly composed of dunite at the boundary between the crust and the mantle. From the depth variation of whole rock and mineral science composition, it was found that the process of formation of dunite by the reaction of harzburgite and basaltic melt is recorded. Moreover, from the physical analysis of the core, the seismic velocity of the mantle that has undergone serpentinization is much lower than that of the lower crust.

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  • Redox state of mantle wedge inferred from the mantle section of the Oman ophiolite

    Grant number:26610173

    2014.4 - 2017.3

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Challenging Exploratory Research

    Research category:Grant-in-Aid for Challenging Exploratory Research

    Awarding organization:Japan Society for the Promotion of Science

    Takazawa Eiichi, SATISH-KUMAR M, AKASAKA Masahide

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    Authorship:Principal investigator  Grant type:Competitive

    Grant amount:\3770000 ( Direct Cost: \2900000 、 Indirect Cost:\870000 )

    We studied the spatial distribution of oxygen fugacity in the Fizh mantle section of the northern Oman ophiolite as an analog for the redox state of mantle wedge. The delta log fO2 relative to FMQ buffer of harzburgites and dunites were calculated following the method of Ballhaus et al. (1991). The values range from FMQ-3.3 to +1.8 and tend to decrease from the crust-mantle boundary (Moho) to the basal part of the mantle section. Dunites are more oxidized than harzburgites. The Fe3+/∑Fe ratio of spinel were evaluated by Mossbauer spectroscopy. The difference is negligible compared to the whole range. The V/Sc and Zn/Fe ratios of whole rock peridotites show a strong negative and positive correlations with delta log fO2 (FMQ), respectively, indicating the observed variation and tendency of delta log fO2 (FMQ) are consistent with residues formed by flux melting of mantle section with a reduced melt/fluid derived from subducted sediment.

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  • 初期島弧における海洋リソスフェアの再融解とボニナイトの生成に関する地質学的検証

    2007.4 - 2010.3

    System name:科学研究費 基盤研究 (C)

    Awarding organization:日本学術振興会

    高澤 栄一

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    Authorship:Principal investigator  Grant type:Competitive

    Grant amount:\4550000 ( Direct Cost: \3500000 、 Indirect Cost:\1050000 )

    オマーンオフィオライト北部に位置するフィズ岩体マントルセクションに分布するかんらん岩類と貫入岩類の構造と化学組成を分析し、中央海嶺における海洋リソスフェアの形成から海洋デタッチメントによる初期島弧での改変のプロセスを明らかにした。とくに融け残りかんらん岩の組成分布から海嶺セグメント構造が見いだされた。海嶺セグメント境界には高枯渇のハルツバージャイトとダナイトが分布し,海洋リソスフェアのデタッチメントに伴い,多量の流体が流動したことが明らかになった。

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  • Comparative study of oceanic plate and ophiolite based on accurate analyses of crustal and mantle material

    Grant number:17340162

    2005 - 2007

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B)

    Research category:Grant-in-Aid for Scientific Research (B)

    Awarding organization:Japan Society for the Promotion of Science

    MIYASHITA Sumio, TAKAZAWA Eiichi, MAEDA Jin-ichiro

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    Grant amount:\15700000 ( Direct Cost: \14800000 、 Indirect Cost:\900000 )

    The results obtained from this research project are summarized as follows.
    Systematic mineral and bulk rock analyses for mantle harzburgites sampled from extensive area of the northern Oman ophiolite indicate that a highly depleted zone is present within the mantle section. The depleted zone is defined by the appearance of Cr-spinels with high Cr# (Cr/(Cr+Al), and traced along the shear zone trending NW-SE described by French group. Remelting of mantle sections caused by invasion of fluids expelled from the underling basement during oceanic thrusting movement would bring a such depleted zone.
    We have examined a regional variation of the mantle-crust transition zone. Lithologic column obtained from7 routes, located at different locations in a segment architecture, indicate a systematic variation of the mantle-crust transition zone depending on the segment structure, as follows. The thickness of the transition zone thickens toward the segment center, and become to thin at the segment margin. However, abnormally thick transition zone was found from the northern tribute branch of Wadi Fizh, locating at the most margin of the segment. Systematic variations in structural features in the transition zone are also obvious, that is, intensive lineation and foliation are well observed at the segment center, while they are only poorly developed at the segment margin. These results suggest that mantle upwelling and magmatic flowage were more vigorous at the segment center. Also lithologic column for extrusive successions are studied at different localities in terms of segment structure. Systematic variations in respect to mode of occurrence of the extrusives were found, as follows: Massive flows are predominant at the segment center with numerous numbers of unit. Whereas, pillow lavas are predominant at the segment margin and are characterized by much thicker unit than the segment center. Thus, both extrusives in the uppermost level, and deeper section of the crust, were controlled by segmentation structure.

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  • Geological Study of Partial Melting of Mafic Rock-Bearing Heterogeneous Upper Mantle

    Grant number:16540413

    2004.4 - 2006.3

    System name:Grant-in-Aid for Scientific Research (C)

    Research category:Grant-in-Aid for Scientific Research (C)

    Awarding organization:Japan Society for the Promotion of Science

    TAKAZAWA Eiichi

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    Authorship:Principal investigator  Grant type:Competitive

    Grant amount:\3400000 ( Direct Cost: \3400000 )

    This research investigated the partial melting and mantle-melt reaction occurred in the Horoman peridotite on the basis of field occurrence and major and trace element abudances in mafic rocks. As a result of study, Type I mafic granulite of the Horoman peridotite were experienced remelting event about 80 million years ago. The center of the mafic layer may have been garnet clinopyroxenite while the margin was a primitive melt in equilibrium with the center in terms of trace elements. Both are now metamorphosed into mafic granulite during uplifting of the Horoman peridotite.
    Following this study, I investigated the mantle section of the Oman ophiolite in 2004-2005 to understand formation of chemical heterogeneity by partial melting of oceanic upper mantle. Detailed analysis of mineral compositions of peridotite samples revealed the presence of highly refractory peridotite zone that obliquely crosscuts the mantle section parallel to the low temperature shear zone. It is advocated that the refractory zone formed by remelting of harzburgite due to reduction of solidus temperature as a result of fluid flow along shear zone.
    Third, heterogeneity of oceanic upper mantle was directly examined using peridotite samples drilled at Mid-Atlantic Ridge in 14°N〜16°N during ODP Leg 209. Optical investigation under microscope and analysis of mineral compositions for drilled cores from Hole B, Site 1271showed that melt flow and mantle-melt reaction in shallowest upper mantle produced a series of lithologies such as impregnated dunite, olivine gabbro, gabbronorite and troctolite as hybrid rocks between dunite and mafic melt.

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  • Geological Study of Partial Melting of Mafic Rock-Bearing Heterogeneous Upper Mantle

    Grant number:16540413

    2004 - 2005

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)

    Research category:Grant-in-Aid for Scientific Research (C)

    Awarding organization:Japan Society for the Promotion of Science

    TAKAZAWA Eiichi

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    Grant amount:\3400000 ( Direct Cost: \3400000 )

    This research investigated the partial melting and mantle-melt reaction occurred in the Horoman peridotite on the basis of field occurrence and major and trace element abudances in mafic rocks. As a result of study, Type I mafic granulite of the Horoman peridotite were experienced remelting event about 80 million years ago. The center of the mafic layer may have been garnet clinopyroxenite while the margin was a primitive melt in equilibrium with the center in terms of trace elements. Both are now metamorphosed into mafic granulite during uplifting of the Horoman peridotite.
    Following this study, I investigated the mantle section of the Oman ophiolite in 2004-2005 to understand formation of chemical heterogeneity by partial melting of oceanic upper mantle. Detailed analysis of mineral compositions of peridotite samples revealed the presence of highly refractory peridotite zone that obliquely crosscuts the mantle section parallel to the low temperature shear zone. It is advocated that the refractory zone formed by remelting of harzburgite due to reduction of solidus temperature as a result of fluid flow along shear zone.
    Third, heterogeneity of oceanic upper mantle was directly examined using peridotite samples drilled at Mid-Atlantic Ridge in 14°N〜16°N during ODP Leg 209. Optical investigation under microscope and analysis of mineral compositions for drilled cores from Hole B, Site 1271showed that melt flow and mantle-melt reaction in shallowest upper mantle produced a series of lithologies such as impregnated dunite, olivine gabbro, gabbronorite and troctolite as hybrid rocks between dunite and mafic melt.

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  • Geological study of interaction between lithospheric mantle and asthenosphere

    Grant number:14540421

    2003.4 - 2005.3

    System name:Grant-in-Aid for Scientific Research (C)

    Research category:Grant-in-Aid for Scientific Research (C)

    Awarding organization:Japan Society for the Promotion of Science

    TAKAZAWA Eiichi

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    Authorship:Principal investigator  Grant type:Competitive

    Grant amount:\4100000 ( Direct Cost: \4100000 )

    This research investigated the mantle-melt reaction that occurs at Earth's extensional environments such as continental rift and mid-ocean ridge. The studied fields includes the Horoman peridotite complex in the Hidaka Metamorphic Belt, Hokkaido, Japan and the mantle section of the Oman ophiolite. On the basis of spatial variation of trace elements such as rare earth elements in the mantle peridotites and in their constituent minerals the reaction between lithospheric mantle and ascending asthenospheric melt was quantitatively modeled. The study showed that the Horoman peridotite are highly heterogeneous in a meter scale so that even in the 140 meters section fertile Iherzolite with primitive mantle composition and depleted harzburgite are observed. The variation of incompatible elements are further complicated thereby showing the metasomatism by asthenospheric melt flow. On the other hand, the mantle section of the Oman ophiolite are more homogeneous in the scale of ten kilo meters. Abundances of major and trace element in the area of 25 x 15km^2 in the Oman mantle section are less variable than those in the 140m section of the Horoman peridotite. Compositional variations in the mantle section of the Oman ophiolite are mainly explained by partial melting and melt extraction beneath mid-ocean ridge. However, this research found greater variations in the Oman ophiolite than it has been known before. These heterogeneities may have formed by remelting and refertilization of oceanic lithospheric mantle in a scale of km.

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  • Geological study of interaction between lithospheric mantle and asthenosphere

    Grant number:14540421

    2002 - 2003

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (C)

    Research category:Grant-in-Aid for Scientific Research (C)

    Awarding organization:Japan Society for the Promotion of Science

    TAKAZAWA Eiichi

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    Grant amount:\4100000 ( Direct Cost: \4100000 )

    This research investigated the mantle-melt reaction that occurs at Earth's extensional environments such as continental rift and mid-ocean ridge. The studied fields includes the Horoman peridotite complex in the Hidaka Metamorphic Belt, Hokkaido, Japan and the mantle section of the Oman ophiolite. On the basis of spatial variation of trace elements such as rare earth elements in the mantle peridotites and in their constituent minerals the reaction between lithospheric mantle and ascending asthenospheric melt was quantitatively modeled. The study showed that the Horoman peridotite are highly heterogeneous in a meter scale so that even in the 140 meters section fertile Iherzolite with primitive mantle composition and depleted harzburgite are observed. The variation of incompatible elements are further complicated thereby showing the metasomatism by asthenospheric melt flow. On the other hand, the mantle section of the Oman ophiolite are more homogeneous in the scale of ten kilo meters. Abundances of major and trace element in the area of 25 x 15km^2 in the Oman mantle section are less variable than those in the 140m section of the Horoman peridotite. Compositional variations in the mantle section of the Oman ophiolite are mainly explained by partial melting and melt extraction beneath mid-ocean ridge. However, this research found greater variations in the Oman ophiolite than it has been known before. These heterogeneities may have formed by remelting and refertilization of oceanic lithospheric mantle in a scale of km.

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  • かんらん岩からマントルプロセスを読む-新たな展開と第4回国際レルゾライト会議をめざして

    Grant number:13894015

    2001

    System name:科学研究費助成事業 基盤研究(C)

    Research category:基盤研究(C)

    Awarding organization:日本学術振興会

    小畑 正明, 小澤 一仁, 新井田 清信, 荒井 章司, 高橋 奈津子, 高澤 栄一

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    Grant amount:\3400000 ( Direct Cost: \3400000 )

    2001年7月21日から25日にわたって,北海道様似町の様似町公民館及びアポイ山荘会議室にてシンポジウム「かんらん岩とマントルプロセス」を開催した.本集会は2002年8-9月北海道様似町で開催予定の第4回国際ワークショップ「造山帯レルゾライトとマントルプロセス」に向けて国内の準備体制を強化し,国内の研究をより一層推進するためのものであった.21日,22日及び23日の夜間は室内講演会,討論会を行った.また23日,24日は幌満かんらん岩の野外地質巡検を実施した.全国の大学から教官21名,学生,院生11名の計32名が参加し,室内討論会では19編の口頭発表と7編のポスターの発表がなされた.カバーしたテーマは岩石学,構造地質学・実験岩石学・微量元素・同位体地球化学,地球物理学,など多方面にわたり,短期間であったが集中的な討議ができた.野外地質巡検では,2002年の本会議の時の巡検予定コースを実地に検討することで幌満かんらん岩の研究の最前線を野外で検証し知識を参加者間で共有する事ができた.25日は関係者で準備委員会を行い,様似町側と詳細な準備打ち合わせを行った.なお本シンポジウムで発表された講演の要旨は別に冊子にまとめ参加者,関係者に配布するべく3月現在準備中である.
    9月下旬には金沢において準備委員会を開催し,本会議のセカンドサーキュラーの骨子を作成,その後関係者間で協議を続けることにより,11月にセコンドサーキュラーを完成させweb上で公開するとともに,世界に配布した・またこの間海外の組織科学プログラムメンバーとも意見を交わし,会議のプロシーディングをJ.Petrolgyに出すこと,またそのゲストエディターのメンバーを決定し2002年の国際会議に向けて準備を大きく進めることができた.

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  • Generation and reorganization of Oman oceanic crust-mantle

    Grant number:11691121

    1999 - 2000

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (A).

    Research category:Grant-in-Aid for Scientific Research (A).

    Awarding organization:Japan Society for the Promotion of Science

    ARAI Shoji, UMINO Susumu, TAKAZAWA Eiichi, MIYASHITA Sumio, MIZUTA Toshio, MASUDA Toshiaki

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    Grant amount:\20000000 ( Direct Cost: \20000000 )

    1. We recognized a wide petrographical variation of peridotite, its deformational history, cystallographical change of minerals and origin of mylonites within the upper mantle section of the northern Oman ophiolite. High-PGE chromitite was also discovered.
    2. We classified the late-intrusive rocks into three types in terms of petrography. Komatititic extrusives were found associated with picrite basalt, a quench phase of the late intrusives.
    3. The segmetation structure of a mid-ocean ridge was estimated by the strutural change of gabbroic layers. Noritic gabbro intruding around the derivative magma chmabers around the segment center impose contact metamorphism of up to granulite facies on surrounding sheeted dike complex. The structure and evolutional history of the roof zone of magma chambers were clarified.
    4. The upper lavas can be classified into three groups by high-accuracy chemical analysis of their Cpx phenocrysts, and the genesis was estimated for individual groups. Boninite was newly found. Preliminary data on the Salahi volcanics that erupted at the obuduction stage were presented.
    5. Hysrothermal metal mineralization was geologically and geochemically examined to understand its genesis. Reaction between aqueous fluid and chlorite in meta-basalts is of vital importance for their characteristics of Zn and Ni contents. The water/rock ratio in the hydrothermal fluid formation is around 20, that is far higher than the calculated values, 2 to 4.
    6. The thermal structure of the ocean-floor metamorphism was examined in basalt to dolerite to confirm a temprature increase downward.
    7. The shear sense on the metamorphic sole is NE-SW and the hanging side was confirmed to have moved toward SW.The basic amphibolite of the sole demonstrates variable flow textures within several tens of meters from the contact with overlying ultramafic rocks.

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  • PRIMARY FORMATION AGES AND CIRCUMUSTANCES OF PRECRETACEOUS ROCKS MAKING UP THE RYOKE BELT IN HONSHU ARC

    Grant number:10440139

    1998 - 2000

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for Scientific Research (B).

    Research category:Grant-in-Aid for Scientific Research (B).

    Awarding organization:Japan Society for the Promotion of Science

    KAGAMI Hiroo, SHIMURA Toshiaki, TAKASAWA Eiichi, KOBAYASHI Kenta, TAINOSHO Yoshiaki, TOYOSHIMA Tsuyoshi

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    Grant amount:\13000000 ( Direct Cost: \13000000 )

    Crustal evolution of the Ryoke Belt is as follows ; (1) 2000-1800Ma.Granitic upper crust was formed from depleted mantle-origin lower crust, which is a primitive basement of the Ryoke Belt. These age data were obtained from Nd model ages of sedimentary-origin metamorphic rocks and granites, which were calculated using depleted mantle parameters, and U-Pb zircons contained in Cretaceous Ryoke granites and Jurassic mafic rocks. (2) 1750-1600Ma. Ceologic events of this age range are not clear. These age data were obtained from Nd model calculations of sedimentary-origin metamorphic rocks and granites. (3)220-190Ma. Mafic volcanism and plutonism took place under continental circumustances. These magmas were derived from continental lithospheric mantle. Age data of this range were measured using Sm-Nd whole rock isochron and whole rock-mineral isochron of gabbros and metadiabases. (4) 170-160Ma. Some mafic to intermediate rocks were formed during this age range. Age data of this range were obtained from Sm-Nd and Rb-Sr whole rock isochrons and Sm-Nd whole rock-mineral isochron. (5) 125-70Ma. Voluminous felsic igneous activity took place during this age ranges under island arc and continental margin circumustances. These age data were obtained from Rb-Sr whole rock isochron. Sm-Nd and Rb-Sr whole rock-mineral isochronos. As initial Sr and Nd isotopic compositions of these rocks are the same as the 220-190Ma mafic rocks, the felsic magmas are considered to have derived from the continental lithosphere lower crust and upper mantle.
    The Cretaceous to Paleogene igneous rocks showing the same isotopic features with Ryoke felsic igneous rocks are widely distributed in the Honshu Arc, which means that the Ryoke-type continental lithosphere basically made up the Honshu Arc.

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  • Geodynamics of generation of oceanic crust-an example of the Oman ophiolite

    Grant number:09041101

    1997 - 1998

    System name:Grants-in-Aid for Scientific Research Grant-in-Aid for international Scientific Research

    Research category:Grant-in-Aid for international Scientific Research

    Awarding organization:Japan Society for the Promotion of Science

    MIYASHITA Sumio, TAKAZAWA Eiichi, ISHIKAWA Tsuyoshi, UMINO Susumu

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    Grant amount:\17700000 ( Direct Cost: \17700000 )

    The results obtained from this research project are summarized for each group.
    Mantle group clarified an interaction between melt and mantle in the mantle-crust transition zone. Also they round the interaction was quite hetrogenous palce to place. Analyses of spinel using river sand show that the mantle peridotites of the Oman ophiolite are highly depleted compared to oceanic mantle, suggesting that signiricant modification or the mantle peridotite occured during later island arc stage.
    Gabbro group round two series of gabbros previously regarded as successive complex, which were formed at advancing and dying magma chambers beneath ocean ridges, respectively. This is explained by overlapping ocean ridges where propagation and retreating or ridges appeared. The central part of ridge segment where thick Moho transition zone occurs was determined through regional detailed geological mapping in the northern Oman ophiolite. From the central part to the tip or ridge segmenl, mineral compositions or layered gabbro varies systematically from less evolved to more evolved compositions.
    Upper crust group measured direction and thickness of dikes from extensive area in the northern Oman ophiolite. They found that the direction of dikes varies for each several km length, indicating the smallest order of segmentation of ocean ridges. The thickness of dikes increases from the central part to tip of the ridge segment in more large scale which is presumed from the petrological features of gabbro and mantle peridotite.
    Structural group found two different mineral lineations on foliation plane in the metamorphic sole beneath the Oman ophiolite. Also they clarified that the degree of preferred orientation is quite various even in one outcrop.

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Teaching Experience

  • Earth Science todayI

    2024
    Institution name:新潟大学

  • 佐渡学概論:佐渡島の自然と人々の営み

    2024
    Institution name:新潟大学

  • 海外フィールド科学実習A

    2023
    Institution name:新潟大学

  • 海外フィールド体験実習

    2023
    Institution name:新潟大学

  • 海外フィールド科学実習B

    2023
    Institution name:新潟大学

  • 地球環境フィールド科学演習

    2023
    Institution name:新潟大学

  • フィールド産業インターンシップ

    2023
    Institution name:新潟大学

  • 地球環境科学特論

    2023
    Institution name:新潟大学

  • 理学基礎演習

    2022
    Institution name:新潟大学

  • 基礎英語コミュニケーション

    2022
    Institution name:新潟大学

  • 理学スタディ・スキルズ

    2022
    Institution name:新潟大学

  • 実践英語コミュニケーション

    2022
    Institution name:新潟大学

  • 地球深部物質論

    2021
    Institution name:新潟大学

  • 台湾スプリングセミナー I

    2021
    Institution name:新潟大学

  • 台湾スプリングセミナー II

    2021
    Institution name:新潟大学

  • 地球科学特別講義I

    2021
    -
    2022
    Institution name:新潟大学

  • 野外実習I

    2021
    Institution name:新潟大学

  • 課題研究(地質科学)

    2020
    Institution name:新潟大学

  • 論文講読演習

    2020
    Institution name:新潟大学

  • 専門力アクティブ・ラーニング

    2020
    -
    2021
    Institution name:新潟大学

  • 先端科学技術総論

    2020
    Institution name:新潟大学

  • 自然科学総論Ⅴ

    2020
    Institution name:新潟大学

  • 地質調査法実習III

    2019
    Institution name:新潟大学

  • 岩石学C

    2019
    Institution name:新潟大学

  • 野外実習A

    2019
    Institution name:新潟大学

  • 野外実習B

    2019
    Institution name:新潟大学

  • 鉱物・岩石学入門

    2018
    Institution name:新潟大学

  • 理学スタディ・スキルズ

    2018
    -
    2022
    Institution name:新潟大学

  • 地質学入門a

    2017
    Institution name:新潟大学

  • 地学基礎実習a

    2017
    Institution name:新潟大学

  • フィールド体験実習

    2017
    Institution name:新潟大学

  • 総合力アクティブ・ラーニング

    2017
    Institution name:新潟大学

  • Earth Science todayⅡ

    2017
    Institution name:新潟大学

  • 地学基礎実習b

    2017
    Institution name:新潟大学

  • 岩石学実験II

    2016
    Institution name:新潟大学

  • 論文作成演習D

    2014
    Institution name:新潟大学

  • 地球科学特別講義III

    2014
    Institution name:新潟大学

  • 地球科学特定研究Db

    2014
    Institution name:新潟大学

  • 岩石学実験I

    2013
    Institution name:新潟大学

  • 台湾スプリングセミナー I

    2013
    -
    2018
    Institution name:新潟大学

  • 台湾スプリングセミナー II

    2013
    -
    2018
    Institution name:新潟大学

  • 地球科学特定研究Dc

    2013
    -
    2015
    Institution name:新潟大学

  • 学術発表演習D

    2013
    -
    2014
    Institution name:新潟大学

  • 中間発表D

    2013
    -
    2014
    Institution name:新潟大学

  • グローバルミーティング

    2013
    Institution name:新潟大学

  • プロジェクト研究特別概説

    2013
    Institution name:新潟大学

  • リサーチインターンシップ

    2013
    Institution name:新潟大学

  • 課題研究(地質科学科)

    2012
    -
    2016
    Institution name:新潟大学

  • 学術発表演習M

    2012
    -
    2015
    Institution name:新潟大学

  • 地球科学特定研究Ma

    2012
    -
    2015
    Institution name:新潟大学

  • 地球科学演習D

    2012
    -
    2015
    Institution name:新潟大学

  • 地球科学演習Ma

    2012
    -
    2015
    Institution name:新潟大学

  • 地球科学特定研究Mb

    2012
    -
    2014
    Institution name:新潟大学

  • 地球科学演習Mb

    2012
    -
    2014
    Institution name:新潟大学

  • 中間発表M

    2012
    -
    2014
    Institution name:新潟大学

  • 地球科学特定研究Da

    2012
    -
    2013
    Institution name:新潟大学

  • 海洋地質学

    2012
    -
    2013
    Institution name:新潟大学

  • リサーチキャンプ

    2012
    Institution name:新潟大学

  • 海洋地殻生成論

    2012
    Institution name:新潟大学

  • 自然構造科学演習MⅠ

    2012
    Institution name:新潟大学

  • 論文作成演習M

    2012
    Institution name:新潟大学

  • 自然構造科学特定研究MⅠ

    2012
    Institution name:新潟大学

  • 岩石学A

    2011
    Institution name:新潟大学

  • セミナー

    2010
    Institution name:新潟大学

  • 岩石学B

    2010
    Institution name:新潟大学

  • 課題研究

    2010
    -
    2023
    Institution name:新潟大学

  • 地球物理学

    2008
    Institution name:新潟大学

  • 野外実習III

    2008
    -
    2018
    Institution name:新潟大学

  • 海底地質学

    2008
    -
    2010
    Institution name:新潟大学

  • 地質調査法II

    2007
    Institution name:新潟大学

  • 地質調査法I

    2007
    Institution name:新潟大学

  • 地質調査法実習II

    2007
    Institution name:新潟大学

  • 地質調査法実習I

    2007
    Institution name:新潟大学

  • マントル・地殻ダイナミクス

    2007
    Institution name:新潟大学

  • 地球化学分析法

    2007
    Institution name:新潟大学

  • 地学概論A

    2007
    Institution name:新潟大学

  • 野外実習I

    2007
    -
    2021
    Institution name:新潟大学

  • 地史学原理

    2007
    -
    2017
    Institution name:新潟大学

  • 地球深部物質論

    2007
    -
    2017
    Institution name:新潟大学

  • 野外実習II

    2007
    -
    2017
    Institution name:新潟大学

  • 地学実験C

    2007
    -
    2016
    Institution name:新潟大学

  • スタディ・スキルズ(地質科学学習法)

    2007
    -
    2016
    Institution name:新潟大学

  • 固体地球化学

    2007
    -
    2013
    Institution name:新潟大学

  • 鉱物学A

    2007
    -
    2012
    Institution name:新潟大学

  • 鉱物学B

    2007
    -
    2012
    Institution name:新潟大学

  • 生きている地球

    2007
    -
    2011
    Institution name:新潟大学

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