| Title Transcription | オキト ドウゴ トウブ ニ ブンプ スル トキバリヤマ ルイソウ オヨビ グンルイソウ ノ ソウジョ ト コウゾウ
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| Title Alternative (English) | The Tokibariyama and Kori Formations in the eastem part of the Oki-Dogo Island
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| File | |
| language |
jpn
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| Author |
Yamamoto, Hiroki
Komuro, Hiroaki
Murakami, Hisashi
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| Description | The Tokibariyama Formation of Oligocene is divided into the Uzuki Rhyolitic and Oku Andesitic Members in ascending order．These members consit mainly of rhyolitic pyroclastic rocks and andesite lavas，respectively．Some thin beds of sandstone or conglomerate are intercalated．This formation generally strikes NE～NNE and dips eastward．The Kori Formation of Miocene unconformably covering the Tokibariyama Formation consists of acidic tuff，sandstone，conglomerate and basalt lava．
These formations are cut by NNE-SSW～NE−SW and NW-SE faults and are bended due to the NESW monocline．This monocline continues to the NW-SE fault southward．Some dikes intrude concordantly with these faults． |
| Journal Title |
島根大学地球資源環境学研究報告
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| Volume | 14
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| Start Page | 101
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| End Page | 108
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| ISSN | 13439774
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| Published Date | 1995-12-25
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| NCID | AA11455176
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| Publisher | 島根大学総合理工学部地球資源環境学教室
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| Publisher Aalternative | Department of Geoscience, Interdisciplinary Faculty of Science and Engineering, Shimane University
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| NII Type |
Departmental Bulletin Paper
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| OAI-PMH Set |
Interdisciplinary Graduate School of Science and Engineering
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| Remark | 12-14,16+ / 1993+
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| 他の一覧 |
