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ID 6519
Title Transcription
マツエソウ ゲンブガンルイ ノ キサイ ガンセキガクテキ ケンキュウ
Title Alternative (English)
Petrological characteristics of Matsue basalt from the Matsue formation, Shimane Prefecture, southwest Japan
File
language
jpn
Attribute
Natural Science
Author
Tsubota, Tomoyuki
Akiyoshi, Hiroyuki
Description
Matsue basalt formed by the mainly alkaline basaltic volcanic activity of the Miocene, located in the central part of Matsue city, Shimane prefecture, southwest Japan. Matsue basalt can be classified into the six groups of lava bodies shown below by field survey and texture and mineral assemblage on the microscope. There are Chausuyama basalt, Hanamagari basalt, Agenogi basalt, Tsuda basaltic andesite, Tohkodai andesite and Rakuzan basaltic andesite bodies. And Matsue basalt became clear that the five rock types exists in Petrology (mineral assemblage). That is three basalts (Chausuyama, Hanamagari and Agenogi basalts), one basaltic andesite (Tsuda and Rakuzan) and one andesite (Tohkodai andesite).That is Tsuda and Rakuzan basaltic andesites have the same petrological character. Futhermore, chromian spinel was found out from Chausuyama and Agenogi basalts.
Journal Title
島根大学教育学部紀要
Volume
41
Start Page
171
End Page
177
ISSN
18808581
Published Date
2007-12-25
NCID
AA12171265
DOI(SelfDOI)
Publisher
島根大学教育学部
Publisher Aalternative
Faculty of Education Shimane University
NII Type
Departmental Bulletin Paper
Format
PDF
Text Version
出版社版
OAI-PMH Set
Faculty of Education
Remark
39-41+ / 2006-2007
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