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メランジュの堆積時および後堆積時の中視的変形構造に関する一解析 : 四国東部秩父累帯南帯の例
https://tokushima-u.repo.nii.ac.jp/records/2010459
https://tokushima-u.repo.nii.ac.jp/records/2010459945c64fe-3d95-4d94-b39d-fb835f83df82
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
trgj_34_95.pdf (518 KB)
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| Item type | 文献 / Documents(1) | |||||||||||
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| 公開日 | 2022-11-09 | |||||||||||
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| アクセス権 | open access | |||||||||||
| 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 | journal article | |||||||||||
| 出版社版DOI | ||||||||||||
| 識別子タイプ | URI | |||||||||||
| 関連識別子 | http://struct.geosociety.jp/pub/trgj/34/3411.pdf | |||||||||||
| 出版タイプ | ||||||||||||
| 出版タイプ | VoR | |||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||
| タイトル | ||||||||||||
| タイトル | メランジュの堆積時および後堆積時の中視的変形構造に関する一解析 : 四国東部秩父累帯南帯の例 | |||||||||||
| 言語 | ja | |||||||||||
| タイトル別表記 | ||||||||||||
| その他のタイトル | Analysis of mesoscopic deformation structures in mélange with special respect to the stages of syn- and post- sedimentation : A case study in the Southern Chichibu Terrane in eastern Shikoku, Southwest Japan | |||||||||||
| 言語 | en | |||||||||||
| 著者 |
石田, 啓祐
× 石田, 啓祐
WEKO
1020
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| 抄録 | ||||||||||||
| 内容記述タイプ | Abstract | |||||||||||
| 内容記述 | In this study, the term "mélange" is used as describing several muddy matrical rocks that are characterized by a chaotic, relatively disturved,"block in matrix" fabric. To find a clue to clarify the origin and the mechanism of the mélanges in the Southern Chichibu Terrane in Southwest Japan, the author examined the analyses of the mesoscopic deformation structures of mélanges at Warabiishi coast in eastern end of Shikoku, where widely crops out the Early Cretaceous succession including muddy chaotic rocks with many blocks of limestone. chert and greenstone. The results can be summarized as follows. 1. The deformation stages of the Warabiishi mélange is subdivided. into three stages. 1) The first stage characterized by rupturing of limestone blocks to form jigsaw-puzzle structure under the condition of high confining- and high pore water- pressures possibly caused by mud-diapirism before the succession of the Warabiishi Unit formed. 2) The second stage is the syn-sedimentary deformations which occur mixing by grabity flows and slidings of non- and semi- consolidated deposits along the lower continental slope to form olistostromes and slump deposits with turbidites. 3) The third stage is the formation of shear structus such as right-stepping en échelon shear fractures (Riedel shear fractures with compressive bridges) and clockwise-back-tilted sigmoidal blocks with ductile shear tails by E-W trending left-lateral simple shearing on condition that the sediments are relatively dewatered and consolidated after the sedimentation of the Warabiishi unit has finished. 2. Based on the sedimentary structures and facies analyses, Warabiishi area of the Southern Chichibu Terrane in Early Cretaceous age is situated in southward inclined lower continental slope with submarine fans where the sediments are supplied by sediment gravity flows as such turbidites and olistostromes partly originated in mud-diapears. 3. The faults controling the formation of southward facing imbricate structure of the Southern Chichibu Terrane moved not only as thrusts but also as E-W trending left-lateral simple shearig faults according to the presence of the above Riedel shear fractures and sigmoidal blocks of the third stage in the Warabiishi mélange along the Butsuzo Tectonic Line. 4. The above-mentioned tectonic features in addition to the southward younging of the mélanges age in the Southern Chichibu Terrane are concordant phenomena with the accretional zone settigs of active convergent margin of the plate tectonics model. |
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| 言語 | en | |||||||||||
| 書誌情報 |
ja : 構造地質 巻 34, p. 95-109, 発行日 1989-04 |
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| 収録物ID | ||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||
| 収録物識別子 | AA11457546 | |||||||||||
| 出版者 | ||||||||||||
| 出版者 | 日本地質学会構造地質研究会 | |||||||||||
| 言語 | ja | |||||||||||
| EID | ||||||||||||
| 識別子 | 74434 | |||||||||||
| 識別子タイプ | URI | |||||||||||
| 言語 | ||||||||||||
| 言語 | jpn | |||||||||||
