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  1. 広島大学の刊行物
  2. Journal of science of the Hiroshima University. Series C, Geology and mineralogy
  3. 7巻3号

Three-Dimensional Size-Analysis of Folds of Quartz Veins in the Psammitic Schist of the Oboke District, Shikoku

https://doi.org/10.15027/53056
https://doi.org/10.15027/53056
bda28e07-5c09-49f4-af65-369b299ec317
名前 / ファイル ライセンス アクション
JSHUC_7-3_125.pdf JSHUC_7-3_125.pdf (4.4 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Three-Dimensional Size-Analysis of Folds of Quartz Veins in the Psammitic Schist of the Oboke District, Shikoku
言語 en
作成者 HARA, Ikuo

× HARA, Ikuo

en HARA, Ikuo

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YOKOYAMA, Shyunji

× YOKOYAMA, Shyunji

en YOKOYAMA, Shyunji

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TSUKUDA, Eikichi

× TSUKUDA, Eikichi

en TSUKUDA, Eikichi

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SHIOTA, Tsugio

× SHIOTA, Tsugio

en SHIOTA, Tsugio

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
内容記述
内容記述 Three-dimensional size-analysis of folds of quartz veins in the psammitic schist of the Oboke district, Shikoku, has been performed. Many of fold-forms observed on the facies of quartz veins show lens-like form elongated along the fold axis, associating bifurcation of folds. A linear relationship is found, between layer-thickness (T) and arc-length (La) as measured on a given joint surface normal to the fold axis and La increases with increase of T. The mode value of La/T ratios is 8-8.5. The La values on individual folds are not always constant as measured on several sections normal to the fold axis, because the folds show commonly lens-like form elongated along the fold axis. The ratios between axial length of fold (Lfa) and T (Lfa/T) appear to show a bimodal distribution, through Lfa tends to increase with increase of T. One of the mode values of Lfa/T ratios is 35 and the other is 65. The small values of Lfa/T ratio tend to be more frequently found on the folds with larger interlimb angles rather than on those with smaller interlimb angles. During the process of growing of amplitude of fold appears to occur frequently the phenomenon that adjacent folds approximately oriented on a straight line are combined with each other into one fold, associating change of La value.
言語 en
出版者
出版者 HIROSHIMA UNIVERSITY
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.15027/53056
ID登録タイプ JaLC
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0075-4374
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA00706718
開始ページ
開始ページ 125
書誌情報 Journal of science of the Hiroshima University. Series C, Geology and mineralogy
Journal of science of the Hiroshima University. Series C, Geology and mineralogy

巻 7, 号 3, p. 125-132, 発行日 1975-10-25
旧ID 53056
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