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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
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
File
language
jpn
Author
Sugawara, Masaru
Iizumi, Shigeru
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
Volume
10
Start Page
53
End Page
56
ISSN
0287816X
Published Date
1991-07-30
NCID
AN00054980
DOI(SelfDOI)
Publisher
島根大学理学部地質学教室
Publisher Aalternative
Department of Geology, Faculty of Science, Shimane University
NII Type
Departmental Bulletin Paper
Format
PDF
Text Version
出版社版
OAI-PMH Set
Faculty of Science and Engineering
Remark
1-11 / 1982-1992
島田昱郎教授退官記念論誌集
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