| ID | 56189 |
| JaLCDOI | |
| Sort Key | 3
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| タイトル（別表記） | Rounded pebble of metamorphosed iron-formations from conglomerate of the Miocene deposits in Yatakayama, Kibi Plateau, Okayama Prefecture
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| フルテキストURL | |
| 著者 |
鈴木 茂之
岡山大学大学院自然科学研究科
小網, 晴男
岡山県立岡山朝日高等学校
臼井, まゆみ
富士学院
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| 抄録 | The Kibi Plateau was a part of the Eurasian Continent and separated by the event of opening of Japan Sea. The rounded pebble which is considered to be continental origin was discovered. The pebble is siliceous and attracts magnets. Prepared thin-sections were observed under microscope. Selected minerals were analyzed by EPMA. The rock is composed of recrystallized quartz, magnetite, riebeckite, stilpnomelane and associated with very tiny minerals with very high relief and interference colors. The assemblage suggests that there is a possibility that the rock is a metamorphic rock of iron-formations and derived from continent.
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| キーワード | Continental origin
Miocene conglomerate
rounded pebble
iron-formations
Kibi Plateau
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| 出版物タイトル |
Okayama University Earth Science Report
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| 発行日 | 2017-12-27
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| 巻 | 24巻
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| 号 | 1号
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| 出版者 | 岡山大学理学部地球科学教室
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| 出版者（別表記） | Department of Earth Sciences, Faculty of Science, Okayama University
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| 開始ページ | 1
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| 終了ページ | 4
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| ISSN | 1340-7414
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| NCID | AN10506284
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| 資料タイプ |
紀要論文
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| OAI-PMH Set |
岡山大学
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| 言語 |
日本語
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| 著作権者 | © 2017 by Okayama University Earth Science Reports Editorial Committee All Rights Reserved
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| 論文のバージョン | publisher
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| Eprints Journal Name | esr
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