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山本 貴史 様の 共著関連データベース

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+(A list of literatures under single or joint authorship with "山本 貴史")

共著回数と共著者名 (a list of the joint author(s))

    27: 山本 貴史

    24: 安東 淳一

    11: 富岡 尚敬

    10: 大藤 弘明, 森下 知晃

    5: 竹下 徹, 荒井 駿, 藤本 光一郎, 重松 紀生

    4: セートビッチ トーマス

    3: DAS Kaushik, ブイ ドン, 伊藤 元雄

    2: 前川 寛和, 和田 菜奈絵, 宿野 浩司, 小林 真大, 小畑 正明, 村田 恵子, 村田 雅美, 植松 勝之, 水上 知行, 渡辺 克晃, 真下 茂, 角野 浩史, 谷 健一郎, 鍵 裕之, 陳 黎亮

    1: Dong Bui, GHOSH Gautam, SANKAR Bose, Thomas Czertowicz, ブイ ドング, 上田 匡将, 小林 哲夫, 曽田 祐介, 浦田 義人, 渡邉 克晃, 福島 菜奈絵, 芳川 雅子, 迫田 夜空

発行年とタイトル (Title and year of the issue(s))

    2012: マントル起源のオリビンに記録されている超底歪速度効果の検査(SIT42 P11) [Net] [Bib]
    Exploration of microstructure induced by ultra low strain rate in mantle derived olivine(SIT42 P11) [Net] [Bib]

    2012: マントル起源のオリビンを用いた超低歪速度効果の検証 [Net] [Bib]
    Verification of ultra low strain rate effect on mantle olivine [Net] [Bib]

    2013: かんらん石の衝撃圧縮実験 深発地震震源過程解明に向けての試験的研究 その2 (R13 O 9) [Net] [Bib] [Doi]
    Shock compression experiment of olivine: toward a better understanding of seismogenic processes of deep earthquakes (R13 O 9) [Net] [Bib] [Doi]

    2013: カンラン岩中の変形したオリビンの微細組織観察(SIT38 13) [Net] [Bib]
    Microstructural observation on naturally deformed olivine peridotite (SIT38 13) [Net] [Bib]

    2013: 上部マントル起源のオリビンの微細組織観察から探る超低歪速度効果の検証 [Net] [Bib] [Doi]
    Microstructural observation on naturally deformed olivine: verification of ultra low strain rate effect [Net] [Bib] [Doi]

    2013: 片状組織を有するアンチゴライト蛇紋岩の強度(SCG07 P01) [Net] [Bib]
    Strength of foliated antigorite serpentinite (SCG07 P01) [Net] [Bib]

    2014: オリビンの変形特性に与える超低歪速度効果の検証 [Net] [Bib] [Doi]
    Investigation of ultra low strain rate effect on deformation properties of olivine [Net] [Bib] [Doi]

    2014: オリビンの衝撃圧縮実験 摩擦溶融に先んじて粉砕が起こった！ (SSS32 14) [Net] [Bib]
    Shock compression experiment of olivine Part 3: pulverization occurred before frictional melting (SSS32 14) [Net] [Bib]

    2014: マントル起源かんらん岩捕獲岩中の鉱物境界に発達する微細組織観察 [Net] [Bib] [Doi]
    Ultra fine textures along grain boundaries in nominally fresh mantle xenoliths [Net] [Bib] [Doi]

    2014: マントル起源かんらん岩捕獲岩中の鉱物境界に発達する微細組織観察(SIT40 08) [Net] [Bib]
    Ultra fine textures along grain boundaries in nominally fresh mantle xenoliths (SIT40 08) [Net] [Bib]

    2014: 天然で変形したオリビンの微細組織観察から探る超低歪速度効果の検証(SMP46 08) [Net] [Bib]
    Verification of ultra low strain rate effect from microstructural observation on naturally deformed olivine (SMP46 08) [Net] [Bib]

    2014: 天然のオリビン中に認められる鉄のコットレル雰囲気 [Net] [Bib] [Doi]
    Iron Cottrell atmospheres observed in naturally deformed olivine [Net] [Bib] [Doi]

    2014: 脆性－塑性遷移領域で変形したマントル起源かんらん岩の微細組織 [Net] [Bib] [Doi]
    Microstructure of mantle derived peridotites deformed at brittle ductile transition zone [Net] [Bib] [Doi]

    2014: 蛇紋岩化したオリビン中に発達する鉄の縞状ゾーニングの形成過程 [Net] [Bib] [Doi]
    Formation process of Fe zoning in olivine grain composed of serpentinized peridotite [Net] [Bib] [Doi]

    2014: 蛇紋岩海山を構成する蛇紋岩の形成過程 [Net] [Bib] [Doi]
    Formation process of serpentinite composed of serpentinite seamount [Net] [Bib] [Doi]

    2015: 北イタリアFineroカンラン岩体の塑性変形履歴の解明 [Net] [Bib] [Doi]
    Ductile Deformation history of Finero phlogopite peridotite [Net] [Bib] [Doi]

    2015: 地質学的証拠に基づいたオリビンの塑性変形特性に与える超低歪速度の影響の解明 [Net] [Bib]

    2015: 天然で変形したオリビンの転位芯に認められる鉄の濃集(SIT04 P01) [Net] [Bib]
    Iron concentration around dislocation in naturally deformed olivine (SIT04 P01) [Net] [Bib]

    2016: インド東部Rengali地域に露出する水酸化鉄脈の成因 [Net] [Bib] [Doi]
    Formation process of fault induced iron hydroxide vein exposed in Rengali province, Eastern India [Net] [Bib] [Doi]

    2016: ピナツボカンラン岩の微細組織観察 交代作用及び変形履歴の推定 (SCG57 11) [Net] [Bib]
    Deformation and metasomatic histories of Pinatubo peridotite estimated from microstructural observation (SCG57 11) [Net] [Bib]

    2017: ピナツボカンラン岩ゼノリスの変形履歴(S2 09) [Net] [Bib] [Doi]
    Deformation history of Pinatubo peridotite xenolith inferred from the microstructures (S2 09) [Net] [Bib] [Doi]

    2017: 三重県中央構造線断層帯の発展 断層コアの軟化における意味 (SCG62 05) [Net] [Bib]
    Development of fault zones along the Median Tectonic Line, Mie Prefecture, south west Japan: implication for weakening in the fault core (SCG62 05) [Net] [Bib]

    2018: 三重県中央構造線断層帯の発展 歪の局所化と軟化について (R13 O 15) [Net] [Bib] [Doi]
    Development of the Median Tectonic Line fault zone, Mie Prefecture, southwest Japan: Strain localization and softening (R13 O 15) [Net] [Bib] [Doi]

    2018: 三重県中央構造線断層帯の発展：歪の局所化と軟化について(SCG57 24) [Net] [Bib]
    Development of the Median Tectonic Line fault zone, Mie Prefecture, southwest Japan: Strain localization and softening (SCG57 24) [Net] [Bib]

    2019: 西南日本、三重県の中央構造線断層帯の発展：歪の局所化と軟化についての一解釈(R15 O 10) [Net] [Bib] [Doi]
    Development of the Median Tectonic Line fault zone in Mie prefecture, southwest Japan: A possible interpretation for strain localization and softening (R15 O 10) [Net] [Bib] [Doi]

    2019: 西南日本、三重県の中央構造線断層帯の発展：歪の局所化と軟化についての一解釈(SCG61 06) [Net] [Bib]
    Development of the Median Tectonic Line Fault zone in Mie Prefecture, Southwest Japan : A Possible Interpretation for Strain Localization and Softening (SCG61 06) [Net] [Bib]

    2020: イタリア北部Fineroかんらん岩体中の変形履歴の解明に向けた希ガス分析と微細組織観察 [Net] [Bib] [Doi]
    Noble gases and deformation history of Finero phlogopite peridotite massif, northern Italy [Net] [Bib] [Doi]

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