島根半島大歳産流紋岩中の松脂岩包有岩の岩石学的意義

島根大学教育学部紀要. 自然科学 Volume 3 Page 71-73 published_at 1970-02-28
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Title
島根半島大歳産流紋岩中の松脂岩包有岩の岩石学的意義
Title
Petrological Significance of the Pitchstone Xenolith Included in Plagioliparite from Otoshi District,Shimane Prefecture, Japan
Title Transcription
シマネ ハントウ オオトシ サン リュウモンガン チュウ ノ ショウシガン ホウユウガン ノ ガンセキガクテキ イギ
Creator
Miura Kiyoshi
Source Title
島根大学教育学部紀要. 自然科学
Memoirs of the Faculty of Education, Shimane University. Natural science
Volume 3
Start Page 71
End Page 73
Journal Identifire
ISSN 05869943
Descriptions
Pitchstones are found as xenoliths in the plagioliparite from Otoshi district. Althouth these are weathered to montmorillonite clay in many outcrops, the fresh rocks studied were corrected with difficulty.
In this paper the author wishes to express on the petrological significance of the pitchstone xenolith included in plagioliparite.
Language
eng
Resource Type departmental bulletin paper
Publisher
島根大学教育学部
The Faculty of Education Shimane University
Date of Issued 1970-02-28
Access Rights open access
Relation
[NCID] AN00107941