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椿 純一 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 "椿 純一")

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

    10: 大谷 具幸, 椿 純一

    6: 河野 雅弘

    4: 上田 圭一, 小嶋 智, 新實 拓也

    2: 西田 敦士

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

    2015: 前期更新世までに活動を停止した断層における破砕帯の特徴(SSS28 P02) [Net] [Bib]
    Characteristics of the fault zones of their activities terminated until the Early Pleistocene (SSS28 P02) [Net] [Bib]

    2015: 地質断層である奈良県中央構造線の断層破砕帯の鉱物学的・地化学的特徴(R14 O 14) [Net] [Bib] [Doi]
    Mineralogical and geochemical characteristics of the inactive fault zone of the Median Tectonic Line, Nara Prefecture (R14 O 14) [Net] [Bib] [Doi]

    2016: 中期更新世に活動を停止した断層破砕帯の特徴 紀伊半島中央部の中央構造線の例 (T1 O 3) [Net] [Bib] [Doi]
    Characteristics of the fault zone whose activity was terminated by the middle Pleistocene: An example of the Median Tectonic Line in central part of Kii Peninsula (T1 O 3) [Net] [Bib] [Doi]

    2016: 第四紀後期に活動していない断層における破砕帯の特徴 奈良県大淀町における中央構造線を例として (SSS31 P11) [Net] [Bib]
    Characteristics of the fault zones terminated by the Late Quaternary an example of the Median Tectonic Line in Nara Prefecture (SSS31 P11) [Net] [Bib]

    2017: 活断層と後期更新世に活動を停止した断層における破砕帯の比較 阿寺断層と奈良県中央構造線 (R15 O 3) [Net] [Bib] [Doi]
    Comparison of the active fault zone and the fault zone terminated its activity by the Late Pliocene: the Atera Fault and the Median Tectonic Line in Nara Prefecture (R15 O 3) [Net] [Bib] [Doi]

    2017: 活断層と後期更新世に活動を停止した断層における破砕帯物質の比較研究 阿寺断層と奈良県中央構造線を例として (SSS12 P12) [Net] [Bib]
    Comparative study of the active fault zone and the fault zone terminated its activity by the Late Pliocene –examples of the Atera Fault and the Median Tectonic Line in Nara Prefecture (SSS12 P12) [Net] [Bib]

    2018: 地表付近のみで変位を生じた断層破砕帯の特徴：阿寺断層を例として(SSS08 P32) [Net] [Bib]
    Characteristics of the fault zone slipped only in the near surface: an example of the Atera Fault (SSS08 P32) [Net] [Bib]

    2018: 地表付近の過去数回の変位で生じた断層破砕帯の特徴 阿寺断層を例として (R15 O 13) [Net] [Bib] [Doi]
    Characteristics of the fault zone slipped only in the near surface and in several times: an example of the Atera Fault (R15 O 13) [Net] [Bib] [Doi]

    2019: 阿寺断層において最近数回のみ変位を生じた断層破砕帯の特徴(SSS15 P10) [Net] [Bib]
    Characteristics of the fault zone with only the recent slips in the Atera Fault (SSS15 P10) [Net] [Bib]

    2019: 阿寺断層の極浅部ですべりを生じた断層破砕帯の特徴(R15 O 6) [Net] [Bib] [Doi]
    Characteristics of the shallow fault zone in the Atera Fault (R15 O 6) [Net] [Bib] [Doi]

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