| Title Transcription | ダイセン ナンセイ コウフチョウ ニオケル ヒダタイ ナンエン ノ コセイダイマツ シュウソクタイ エビ コウゾウタイ
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| Title Alternative (English) | The Ebi tectonic zone, Late Paleozoic suture of the southem margln of the Hida Belt in Kofu-cho, southwest of Mt Daisen, Southwest Japan
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| File | |
| language |
jpn
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| Author |
Sugawara, Masaru
Iizumi, Shigeru
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| Description | The late Paleozoic Ebi Tectonic Zone, newly proposed, is a suture zone developed outer margin of the Hida Belしwhich is now bounded by the“Sangun Metamorphic Terrane”of the Chugoku region. It is a zone, consiting of a mylonite granitic rocks and melanges from north to south. The Ebi Granite gradually changes into the mylonite granitic rocks in the Ebi Tectonic Zone, and mylonites vary in granitic rocks, greenstones, and andesites. The melanges embedded clasts of andesites, granitic rocks in a siltstone and tuffaceous sandstone matrix.
The Ebi Tectnic Zone thrust ove｝the pelitic schists of the“Sangun Metamorphic Terrane”. |
| Journal Title |
Geological reports of Shimane University
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| Volume | 10
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| Start Page | 53
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| End Page | 56
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| ISSN | 0287816X
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| Published Date | 1991-07-30
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| NCID | AN00054980
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| DOI（SelfDOI） | |
| Publisher | 島根大学理学部地質学教室
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| Publisher Aalternative | Department of Geology, Faculty of Science, Shimane University
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| NII Type |
Departmental Bulletin Paper
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| Format |
PDF
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| Text Version |
出版社版
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| OAI-PMH Set |
Faculty of Science and Engineering
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| Remark | 1-11 / 1982-1992
島田昱郎教授退官記念論誌集
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| 他の一覧 |
