| File | |
| Title |
大山南西江府町における飛騨帯南縁の古生代末収束帯,江尾構造帯
|
| Title |
The Ebi tectonic zone, Late Paleozoic suture of the southem margln of the Hida Belt in Kofu-cho, southwest of Mt Daisen, Southwest Japan
|
| 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
|
| Creator |
Sugawara Masaru
Iizumi Shigeru
|
| Source Title |
島根大学地質学研究報告
Geological reports of Shimane University
|
| Volume | 10 |
| Start Page | 53 |
| End Page | 56 |
| Journal Identifire |
ISSN 0287816X
|
| Descriptions |
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”. |
| Language |
jpn
|
| Resource Type | departmental bulletin paper |
| Publisher |
島根大学理学部地質学教室
Department of Geology, Faculty of Science, Shimane University
|
| Date of Issued | 1991-07-30 |
| Publish Type | Version of Record |
| Access Rights | open access |
| Relation |
[NCID] AN00054980
|
| Remark | 1-11 / 1982-1992 |
