| ID | 105967 |
| Title Transcription | シコク セイブ チチブタイ トリガタヤマ オオノガハラ セッカイ ガンタイ ト シンキ イノ ヘンセイ コンプレックス ノ チシツ コウゾウ
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| Title Alternative | Geological structures of the Torigatayama-Onogahara limestone and the Younger Ino metamorphic complex of the Chichibu Terrain, West Shikoku
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| Author |
Murata, Akihiro
Institute of Socio-Arts and Sciences, University of Tokushima
Tokushima University Educator and Researcher Directory
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Maekawa, Hirokazu
Department of Physical Science, Graduate School of Science, Osaka Prefectural University
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| Keywords | Torigatayama-Onogahara limestone
geological structures
Younger Ino metamorphic complex
Kurosegawa Terrain
Chichibu Terrain
Shikoku
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| Content Type |
Departmental Bulletin Paper
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| Description | Geological structures of the Torigatayama-Onogahara limestone body of the Permian accretionary complex and the Younger Ino metamorphic complex were studied in the Chichibu Terrain in West Shikoku. The Torigatayama-Onogahara limestone body consists of six limestone bodies, which occur in a convex way toward south. The limestone bodies are northward facing and form southward thrust sheet, and do not occur in the axial part of a synform. An antiform and a synform occur in the distributional area of the Younger Ino metamorphic complex. The antiform does not extend westward to the distributional area of the Yusugawa Unit of the Jurassic accretionary complex. The Permian accretionary complex and the Younger Ino metamorphic complex do not occupy the highest tectonic horizon in the Chichibu Terrain in West Shikoku.
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| Journal Title |
徳島大学総合科学部自然科学研究 = Natural Science Research, The University of Tokushima
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| ISSN | 09146385
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| NCID | AN10065859
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| Volume | 27
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| Issue | 4
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| Start Page | 91
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| End Page | 100
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| Sort Key | 91
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| Published Date | 2013-10
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| EDB ID | |
| FullText File | |
| language |
jpn
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| TextVersion |
Publisher
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| departments |
Science and Technology
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