ID | 61955 |
JaLCDOI | |
Sort Key | 4
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タイトル(別表記) | The Kibi Plateau Surface ― relationship with the Paleogene and Miocene deposits in middle western part of Okayama Prefecture, Japan ―
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フルテキストURL | |
著者 |
田中 元
復建調査設計株式会社岡山支社
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抄録 | The Kibi Plateau Surface is associated with the Paleogene gravel river bed deposits of the Kibi Group and the Miocene marine deposits of the Katsuta Group and the Bihoku Group. These Paleogene and Miocene units are valley fill deposits. The Kibi Group is composed of formations which is deposited by more than 7 different depositional events during earliest to latest Paleogene Period. Repeated cycles of “erosion - formation of new valley system - deposition and fill up the valley” created the low relief topographic surface. The deposition of
the Miocene deposits might complete the Kibi Plateau Surface. Detailed field works have done in middle western part of Okayama Prefecture. The Kibi Plateau Surface in study area is gently dipping from NW (about 600m high) to SE (about 100m high). The distributions of the Paleogene and Miocene deposits fit the surface.
At the southern margin of the Kibi Plateau, the surface is a little inclined (from 400m high to 100m high) where the bottom of paleo-valleys of the Paleogene deposits are subparallel to the surface. It suggests that the gentle tilting of the Kibi Plateau is caused by an up-warping.
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キーワード | Kibi Plateau Surface
Paleogene
Neogene
Miocene
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出版物タイトル |
Okayama University Earth Science Report
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発行日 | 2021-03-31
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巻 | 27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 | 19
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終了ページ | 27
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ISSN | 1340-7414
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NCID | AN10506284
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資料タイプ |
学術雑誌論文
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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 | © 2021 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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NAID | |
Eprints Journal Name | esr
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