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Title Transcription
シコク チュウオウブ サンバガワタイ セバダニ チイキ ニ アタラシク ミイダサレタ エクロジャイト
Title Alternative (English)
Newly found eclogite from the Sambagawa metamorphic belt in the Sebadani area, central Shikoku, Japan
File
language
jpn
Author
Naohara, Ryosuke
Description
ln the Sebadani area of the Sambagawa metamorphic belt,central Shikoku,two types of prograde eclogites have been described so far.One was formed by contact metamorphism by emplacement of a hightemperature eclogite brock,the Sebadani metagabbro mass,and the other was formed by the Sambagawa prograde metamorphism.Two prograde eclogite localities have been newly discovered.The eclogites show
clockwise P-T path,from the epidote-amphibolite facies through the eclogite facies as a peak condition to the epidote-amphibolite facies.This genetic character is same as the other Sambagawa eclogitic schists already described.The cause of increasing temperature up to the eclogite facies condition will be important
for understanding the thermal history of the Sambagawa metamorphism in the Sebadani district.
Journal Title
島根大学地球資源環境学研究報告
Volume
14
Start Page
117
End Page
125
ISSN
13439774
Published Date
1995-12-25
NCID
AA11455176
DOI(SelfDOI)
Publisher
島根大学総合理工学部地球資源環境学教室
Publisher Aalternative
Department of Geoscience, Interdisciplinary Faculty of Science and Engineering, Shimane University
NII Type
Departmental Bulletin Paper
Format
PDF
Text Version
出版社版
OAI-PMH Set
Interdisciplinary Graduate School of Science and Engineering
Remark
12-14,16+ / 1993+
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