| Title Transcription | シマネケン オキグン フセ シュウヘン ノ コダイサンキ トキバリヤマ ルイソウ
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| Title Alternative (English) | The Paleogene Tokibad Fomation around Fuse, Oki Islands
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| File | |
| language |
jpn
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| Author |
Yamauchi, Seiki
Murakami, Hisashi
Nakayama, Katsuhiro
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| Description | The Paleogene Tokibariyama Formation around Fuse，Oki Dogo Island is divided into 7 members．The lowest member is a talus basal conglomerate which shows the facies of sediments at a foot of a steep cliff，and lower members abut agaist steep wall of their basement rocks．These facts show that the sedimentary basin have resulted from depression caused by faulting．Volcanic clasts in debris flow deposits at the upper part of the talus basal conglomerate implies that near the study area any other volcano-pulutonic activity had taken placed prior to sedimentation of the talus basal conglomerate．Probably several volcano-pulutonic activities occured during the Tokibariyama Formation stage．
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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 | 14
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| Start Page | 81
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| End Page | 88
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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 |
