| Title Transcription | コダイサンキ サクラエ コールドロン ナンエンブ ノ チシツ コウゾウ
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| Title Alternative (English) | Geologic structure in the southern marginal area of the Oligocene Sakurae cauldron
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| File | |
| language |
jpn
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| Author |
Hibata, Mika
Ohtani, Takaaki
Komuro, Hiroaki
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| Description | The southern margin of the Sakurae cauldron，previously the last unsurveyed area，has now been studied in detail．The Sakurae cauldron is filled with the Nakano Formation of the Sakurae Group．The lowermost part of the Nakano Formation is exposed in the study area．It consists of rhyolite lava，fine tuff，crystal tuff，lapilli tuff，welded tuff，and andesite lava layers，inascending order．These are in fault contact with the upper Nakano Formation，and the fault probably strikes WNW-ESE．This is a hinge fault，the displacement of which increases toward the SE．The fault-block on the south side is tilted to the north due to the intrusion of the Yagami granodiorite．
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| Journal Title |
島根大学地球資源環境学研究報告
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| Volume | 23
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| Start Page | 49
|
| End Page | 53
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| ISSN | 13439774
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| Published Date | 2004-12-27
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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 |
