ECHIGO Takuya

写真a

Affiliation

Graduate School of International Resource Sciences  Department of Earth Resource Science 

Mail Address

E-mail address

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Research Interests 【 display / non-display 】

  • Mineralogy

  • Earth Science

  • Crystallography

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Graduating School 【 display / non-display 】

  • 1999.04
    -
    2003.03

    University of Tsukuba   First Cluster of College   Department of Natural Sciences   Graduated

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Graduate School 【 display / non-display 】

  • 　
    -
    2008.03

    University of Tsukuba  Graduate School of Life and Environmental Sciences  Division of Earth Evolution Sciences  Doctor's Course  Completed

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Degree 【 display / non-display 】

  • University of Tsukuba -  Ph.D.

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Campus Career 【 display / non-display 】

  • 2015.04
    -
    Now

    Akita University   Abolished organization   Dept. of Earth Resource Science   Associate Professor  

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Research Areas 【 display / non-display 】

  • Natural Science / Solid earth sciences

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Research Achievements 【 display / non-display 】

    ◆Original paper【 display / non-display 】

  • Platinum-group element mineralization in the Merensky Reef of the Limpopo mine, Eastern Limb of the Bushveld Complex, South Africa.

    Maki BIRUKAWA, Yasushi WATANABE, Takuya ECHIGO and Carmela TUPAZ

    International Journal of the Society of Materials Engineering for Resources ( 日本素材物性学会 )  25 ( 2 ) 183 - 188   2022.10  [Refereed]

    Research paper (journal)   Domestic Co-author

  • K–Ar geochronology of orogenic gold mineralization in the Vangtat gold belt, southeastern Laos: Effect of excess argon in hydrothermal quartz

    Patthana Bounliyong, Tetsumaru Itaya, Antonio Arribas, Yasushi Watanabe, Henry Wong, Takuya Echigo

    Resource Geology ( Resource Geology )  71 ( 2 ) 161 - 175   2021.04  [Refereed]

    Research paper (journal)   International Co-author

    DOI

  • Reduction of oxidized sulfur in the formation of the Grasberg porphyry copper-gold deposit, Papua, Indonesia

    Adi Sulaksono, Yasushi Watanabe, Antonio Arribas, Takuya Echigo, Reza Al Furqan, Clyde A. Leys

    Mineralium Deposita ( Mineralium Deposita )    2021.02  [Refereed]

    Research paper (journal)   International Co-author

    DOI

  • Mineralogy and geochemistry of the Berong Ni-Co laterite deposit, Palawan, Philippines

    Carmela Alen Tupaz, Yasushi Watanabe, Kenzo Sanematsu, Takuya Echigo

    Ore Geology Reviews ( Ore Geology Reviews )  125   2020.10  [Refereed]

    Research paper (journal)   Domestic Co-author

    フィリピンのパラワン島に位置するBelong Ni-Co鉱床は、カンラン岩が風化して生成したラテライト鉱床である。本研究では、Belong鉱床の地質学的、地球化学的、鉱物的な調査研究を行い、ガニエライト・Mn水酸化物・ゲーサイトといった鉱物がNiおよびCoの主要なホストであることを明らかにした。

    DOI

  • Ni-Co mineralization in the Intex laterite deposit, Mindoro, Philippines

    Carmela Alen J. Tupaz, Yasushi Watanabe, Kenzo Sanematsu,Takuya Echigo, Carlo Arcilla, Cherisse Ferrer

    Minerals ( MDPI (Multidisciplinary Digital Publishing Institute) )  10 ( 7 ) 1 - 33   2020.07  [Refereed]

    Research paper (journal)   International Co-author

    フィリピンのミンドロ島に位置するIntex Ni-Co鉱床は、輝石を主とする超苦鉄質岩が風化して生成したラテライト鉱床である。本研究では、Intex鉱床の地質学的、地球化学的、鉱物的な調査研究を行い、ガニエライト・Mn水酸化物・ゲーサイトといった鉱物がNiおよびCoの主要なホストであることを明らかにした。

    DOI

    • display all >>

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    ◆Other【 display / non-display 】

  • Volatile components in island arc magma indicated by mineral and melt inclusions in anorthite megacrysts: case study from Ogi peninsula, Sado Island

    Echigo Takuya, Nishimaki Shino, Hoshino Mihoko, Kimata Mitsuyoshi, Shimizu Masahiro, Saito Shizuo, Nishida Norimasa

    Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences ( Japan Association of Mineralogical Sciences )  2017 ( 0 ) 7   2017

    Ca-rich plagioclase (An > 90 %) larger than 10 mm, which is called anorthite megacryst, occurs commonly from basalt - andesite in Japanese Island arc. We investigated anorthite megacrysts from Ogi Peninsula, Sado island and found melt inclusions rich in volatile components such as Cl and S. Electron microprobe analysis show that SiO<sub>2</sub> and Cl in these melt inclusions range 48 - 56% and 0.01 - 0.12%, respectively. Our results indicate that anorthite megacrysts from Ogi Peninsula grew in volatile-rich environment caused by release of Cl and S from subducting slab.

    DOI CiNii Research

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