| Item type |
文献 / Documents(1) |
| 公開日 |
2022-11-10 |
| アクセス権 |
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アクセス権 |
open access |
| 資源タイプ |
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|
資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
|
資源タイプ |
journal article |
| 出版社版DOI |
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|
識別子タイプ |
URI |
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|
関連識別子 |
http://struct.geosociety.jp/pub/trgj/35/3502.pdf |
| 出版タイプ |
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|
出版タイプ |
VoR |
|
出版タイプResource |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
| タイトル |
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|
タイトル |
先新第三系中に発達する鉛直に近い回転軸を持つ様々な形態の摺曲（屈曲） : 中期中新世における西南日本の時計回り回転と関連して |
|
言語 |
ja |
| タイトル別表記 |
|
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その他のタイトル |
Various folds (bends) with subvertical/vertical rotation axes in the pre-Neogene terranes of Southwest Japan : their significances on the Middle Miocene clockwise-rotation of Southwest Japan |
|
言語 |
en |
| タイトル別表記 |
|
|
その他のタイトル |
先新第三系中の鉛直回転軸を持つ摺曲（屈曲） |
|
言語 |
ja |
| 著者 |
狩野, 謙一
小坂, 和夫
村田, 明広
柳井, 修一
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| 抄録 |
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内容記述タイプ |
Abstract |
|
内容記述 |
Various folds (bends) with subvertical/vertical axes are widely developed in the pre-Neogene terranes of Southwest Japan. They are variable in shape, conical folds, accordion folds, megakink bands and so on, and some of them are associated with strike-slip faults. Their size ranges from several meters to 10km or more in half-wavelength. Their deformation style indicate that they were produced under a brittle condition in a shallow level of the crust. They are superimposed on the pre-existing structures, and are regarded to have been formed mostly during the Middle Miocene contemporaneously at the time of the clockwise-rotation of Southwest Japan. The presence of them, thus, suggests that the upper crust of island arc is easily deformable around subvertical/vertical rotation axes to form various folds (bends) and locally strike-slip faults during its rotation. |
|
言語 |
en |
| 書誌情報 |
ja : 構造地質
巻 35,
p. 11-21,
発行日 1990-04
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| 収録物ID |
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|
収録物識別子タイプ |
NCID |
|
収録物識別子 |
AA11457546 |
| 出版者 |
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|
出版者 |
日本地質学会構造地質研究会 |
|
言語 |
ja |
| EID |
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|
識別子 |
61378 |
|
識別子タイプ |
URI |
| 言語 |
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|
言語 |
jpn |
trgj_35_11.pdf (4.13 MB)
